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800 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5de54124-4a60-67d4-28d2-0f7cde9fa3ee | 2.1.1 Observed Warming and its Causes | null | 2 | Human-caused climate change is already affecting many weather and climate extremes in every region across the globe. This has led to widespread adverse impacts on food and water security, human health and on economies and society and related losses and damages to nature and people. | Yes | has led to | E | Positive | Negative_correlation | widespread adverse impacts on water security | damages to nature | in every region across the globe | null | water security | damages to nature | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
801 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5de54124-4a60-67d4-28d2-0f7cde9fa3ee | 2.1.1 Observed Warming and its Causes | null | 2 | Human-caused climate change is already affecting many weather and climate extremes in every region across the globe. This has led to widespread adverse impacts on food and water security, human health and on economies and society and related losses and damages to nature and people. | Yes | has led to | E | Positive | Negative_correlation | widespread adverse impacts on water security | damages to people | in every region across the globe | null | water security | damages to people | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
802 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5de54124-4a60-67d4-28d2-0f7cde9fa3ee | 2.1.1 Observed Warming and its Causes | null | 2 | Human-caused climate change is already affecting many weather and climate extremes in every region across the globe. This has led to widespread adverse impacts on food and water security, human health and on economies and society and related losses and damages to nature and people. | Yes | has led to | E | Positive | Negative_correlation | widespread adverse impacts on human health | losses to nature | in every region across the globe | null | human health | losses to nature | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
803 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5de54124-4a60-67d4-28d2-0f7cde9fa3ee | 2.1.1 Observed Warming and its Causes | null | 2 | Human-caused climate change is already affecting many weather and climate extremes in every region across the globe. This has led to widespread adverse impacts on food and water security, human health and on economies and society and related losses and damages to nature and people. | Yes | has led to | E | Positive | Negative_correlation | widespread adverse impacts on human health | losses to people | in every region across the globe | null | human health | losses to people | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
804 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5de54124-4a60-67d4-28d2-0f7cde9fa3ee | 2.1.1 Observed Warming and its Causes | null | 2 | Human-caused climate change is already affecting many weather and climate extremes in every region across the globe. This has led to widespread adverse impacts on food and water security, human health and on economies and society and related losses and damages to nature and people. | Yes | has led to | E | Positive | Negative_correlation | widespread adverse impacts on human health | damages to nature | in every region across the globe | null | human health | damages to nature | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
805 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5de54124-4a60-67d4-28d2-0f7cde9fa3ee | 2.1.1 Observed Warming and its Causes | null | 2 | Human-caused climate change is already affecting many weather and climate extremes in every region across the globe. This has led to widespread adverse impacts on food and water security, human health and on economies and society and related losses and damages to nature and people. | Yes | has led to | E | Positive | Negative_correlation | widespread adverse impacts on human health | damages to people | in every region across the globe | null | human health | damages to people | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
806 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5de54124-4a60-67d4-28d2-0f7cde9fa3ee | 2.1.1 Observed Warming and its Causes | null | 2 | Human-caused climate change is already affecting many weather and climate extremes in every region across the globe. This has led to widespread adverse impacts on food and water security, human health and on economies and society and related losses and damages to nature and people. | Yes | has led to | E | Positive | Negative_correlation | widespread adverse impacts on economies | losses to nature | in every region across the globe | null | economies | losses to nature | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
807 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5de54124-4a60-67d4-28d2-0f7cde9fa3ee | 2.1.1 Observed Warming and its Causes | null | 2 | Human-caused climate change is already affecting many weather and climate extremes in every region across the globe. This has led to widespread adverse impacts on food and water security, human health and on economies and society and related losses and damages to nature and people. | Yes | has led to | E | Positive | Negative_correlation | widespread adverse impacts on economies | losses to people | in every region across the globe | null | economies | losses to people | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
808 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5de54124-4a60-67d4-28d2-0f7cde9fa3ee | 2.1.1 Observed Warming and its Causes | null | 2 | Human-caused climate change is already affecting many weather and climate extremes in every region across the globe. This has led to widespread adverse impacts on food and water security, human health and on economies and society and related losses and damages to nature and people. | Yes | has led to | E | Positive | Negative_correlation | widespread adverse impacts on economies | damages to nature | in every region across the globe | null | economies | damages to nature | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
809 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5de54124-4a60-67d4-28d2-0f7cde9fa3ee | 2.1.1 Observed Warming and its Causes | null | 2 | Human-caused climate change is already affecting many weather and climate extremes in every region across the globe. This has led to widespread adverse impacts on food and water security, human health and on economies and society and related losses and damages to nature and people. | Yes | has led to | E | Positive | Negative_correlation | widespread adverse impacts on economies | damages to people | in every region across the globe | null | economies | damages to people | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
810 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5de54124-4a60-67d4-28d2-0f7cde9fa3ee | 2.1.1 Observed Warming and its Causes | null | 2 | Human-caused climate change is already affecting many weather and climate extremes in every region across the globe. This has led to widespread adverse impacts on food and water security, human health and on economies and society and related losses and damages to nature and people. | Yes | has led to | E | Positive | Negative_correlation | widespread adverse impacts on society | losses to nature | in every region across the globe | null | society | losses to nature | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
811 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5de54124-4a60-67d4-28d2-0f7cde9fa3ee | 2.1.1 Observed Warming and its Causes | null | 2 | Human-caused climate change is already affecting many weather and climate extremes in every region across the globe. This has led to widespread adverse impacts on food and water security, human health and on economies and society and related losses and damages to nature and people. | Yes | has led to | E | Positive | Negative_correlation | widespread adverse impacts on society | losses to people | in every region across the globe | null | society | losses to people | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
812 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5de54124-4a60-67d4-28d2-0f7cde9fa3ee | 2.1.1 Observed Warming and its Causes | null | 2 | Human-caused climate change is already affecting many weather and climate extremes in every region across the globe. This has led to widespread adverse impacts on food and water security, human health and on economies and society and related losses and damages to nature and people. | Yes | has led to | E | Positive | Negative_correlation | widespread adverse impacts on society | damages to nature | in every region across the globe | null | society | damages to nature | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
813 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5de54124-4a60-67d4-28d2-0f7cde9fa3ee | 2.1.1 Observed Warming and its Causes | null | 2 | Human-caused climate change is already affecting many weather and climate extremes in every region across the globe. This has led to widespread adverse impacts on food and water security, human health and on economies and society and related losses and damages to nature and people. | Yes | has led to | E | Positive | Negative_correlation | widespread adverse impacts on society | damages to people | in every region across the globe | null | society | damages to people | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
814 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q49-B3261C4F-9707-4079-AB1B-E2941B69EB3C | 2.1.2 Observed Climate System Changes and Impacts to Date | 2.1.2.d | 2 | Although overall agricultural productivity has increased, climate change has slowed this growth in agricultural productivity over the past 50 years globally (medium confidence), with related negative crop yield impacts mainly recorded in mid- and low latitude regions, and some positive impacts in some high latitude reg... | Yes | has slowed | E | Positive | Negative_correlation | climate change | slowed growth in overall agricultural productivity | null | over the past 50 years globally | climate change | growth in overall agricultural productivity | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | medium confidence | null |
815 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q49-B3261C4F-9707-4079-AB1B-E2941B69EB3C | 2.1.2 Observed Climate System Changes and Impacts to Date | 2.1.2.d | 2 | Although overall agricultural productivity has increased, climate change has slowed this growth in agricultural productivity over the past 50 years globally (medium confidence), with related negative crop yield impacts mainly recorded in mid- and low latitude regions, and some positive impacts in some high latitude reg... | Yes | impacts | I | Positive | Positive_correlation | slowed growth in overall agricultural productivity | negative crop yield impacts | over the past 50 years globally | in mid latitude regions | growth in overall agricultural productivity | crop yield impacts | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
816 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q49-B3261C4F-9707-4079-AB1B-E2941B69EB3C | 2.1.2 Observed Climate System Changes and Impacts to Date | 2.1.2.d | 2 | Although overall agricultural productivity has increased, climate change has slowed this growth in agricultural productivity over the past 50 years globally (medium confidence), with related negative crop yield impacts mainly recorded in mid- and low latitude regions, and some positive impacts in some high latitude reg... | Yes | impacts | I | Positive | Positive_correlation | slowed growth in overall agricultural productivity | negative crop yield impacts | over the past 50 years globally | in low latitude regions | growth in overall agricultural productivity | crop yield impacts | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
817 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q49-B3261C4F-9707-4079-AB1B-E2941B69EB3C | 2.1.2 Observed Climate System Changes and Impacts to Date | 2.1.2.d | 2 | Although overall agricultural productivity has increased, climate change has slowed this growth in agricultural productivity over the past 50 years globally (medium confidence), with related negative crop yield impacts mainly recorded in mid- and low latitude regions, and some positive impacts in some high latitude reg... | Yes | impacts | I | Positive | Negative_correlation | slowed growth in overall agricultural productivity | some positive crop yield impacts | over the past 50 years globally | in some high latitude regions | growth in overall agricultural productivity | crop yield impacts | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
818 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q49-F98361D4-ADEB-4FB5-8C38-8197072EB778 | 2.1.2 Observed Climate System Changes and Impacts to Date | 2.1.2.d | 6 | Unsustainable agricultural expansion, driven in part by unbalanced diets, increases ecosystem and human vulnerability and leads to competition for land and/or water resources (high confidence). | Yes | driven in part by | E | Positive | Positive_correlation | unbalanced diets | unsustainable agricultural expansion | null | null | unbalanced diets | unsustainable agricultural expansion | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
819 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q49-F98361D4-ADEB-4FB5-8C38-8197072EB778 | 2.1.2 Observed Climate System Changes and Impacts to Date | 2.1.2.d | 6 | Unsustainable agricultural expansion, driven in part by unbalanced diets, increases ecosystem and human vulnerability and leads to competition for land and/or water resources (high confidence). | Yes | increases | E | Positive | Positive_correlation | unsustainable agricultural expansion | increased ecosystem vulnerability | null | null | unsustainable agricultural expansion | ecosystem vulnerability | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
820 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q49-F98361D4-ADEB-4FB5-8C38-8197072EB778 | 2.1.2 Observed Climate System Changes and Impacts to Date | 2.1.2.d | 6 | Unsustainable agricultural expansion, driven in part by unbalanced diets, increases ecosystem and human vulnerability and leads to competition for land and/or water resources (high confidence). | Yes | increases | E | Positive | Positive_correlation | unsustainable agricultural expansion | increased human vulnerability | null | null | unsustainable agricultural expansion | human vulnerability | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
821 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q49-F98361D4-ADEB-4FB5-8C38-8197072EB778 | 2.1.2 Observed Climate System Changes and Impacts to Date | 2.1.2.d | 6 | Unsustainable agricultural expansion, driven in part by unbalanced diets, increases ecosystem and human vulnerability and leads to competition for land and/or water resources (high confidence). | Yes | leads to | E | Positive | Positive_correlation | unsustainable agricultural expansion | competition for land resources | null | null | unsustainable agricultural expansion | competition for land resources | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
822 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q49-F98361D4-ADEB-4FB5-8C38-8197072EB778 | 2.1.2 Observed Climate System Changes and Impacts to Date | 2.1.2.d | 6 | Unsustainable agricultural expansion, driven in part by unbalanced diets, increases ecosystem and human vulnerability and leads to competition for land and/or water resources (high confidence). | Yes | leads to | E | Positive | Positive_correlation | unsustainable agricultural expansion | competition for water resources | null | null | unsustainable agricultural expansion | competition for water resources | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
823 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q31-93e24cdf-4364-9e8e-655c-9c3bc254dead | 2.1.2 Observed Climate System Changes and Impacts to Date | 2.1.2.c | 6 | Impacts on some ecosystems are approaching irreversibility such as the impacts of hydrological changes resulting from the retreat of glaciers, or the changes in some mountain [..] ecosystems driven by permafrost thaw. | Yes | resulting from | E | Positive | Positive_correlation | retreat of glaciers | impacts of hydrological changes | null | null | retreat of glaciers | impacts of hydrological changes | null | impacts on some ecosystems | null | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q16 | medium confidence | No |
824 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q31-93e24cdf-4364-9e8e-655c-9c3bc254dead | 2.1.2 Observed Climate System Changes and Impacts to Date | 2.1.2.c | 6 | Impacts on some ecosystems are approaching irreversibility such as the impacts of hydrological changes resulting from the retreat of glaciers, or the changes in some mountain [..] ecosystems driven by permafrost thaw. | Yes | driven by | E | Positive | Positive_correlation | permafrost thaw | changes in some mountain ecosystems | null | null | permafrost thaw | changes in some mountain ecosystems | null | impacts on some ecosystems | null | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q16 | medium confidence | No |
825 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q101-2da3a440-4ee1-ec4f-b99f-cc456ee2f24e | 2.1.1 Observed Warming and its Causes | 2.1.1.b | 1 | Observed increases in well-mixed GHG concentrations since around 1750 are unequivocally caused by GHG emissions from human activities. Land and ocean sinks have taken up a near-constant proportion (globally about 56% per year) of CO2 emissions from human activities over the past six decades, with regional differences. | Yes | caused by | E | Positive | Positive_correlation | greenhouse gases emissions | increases in well-mixed greenhouse gases concentrations | null | since around 1750 | greenhouse gases emissions | well-mixed greenhouse gases concentrations | null | null | GHG = greenhouse gases | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
826 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q101-2da3a440-4ee1-ec4f-b99f-cc456ee2f24e | 2.1.1 Observed Warming and its Causes | 2.1.1.b | 1 | Observed increases in well-mixed GHG concentrations since around 1750 are unequivocally caused by GHG emissions from human activities. Land and ocean sinks have taken up a near-constant proportion (globally about 56% per year) of CO2 emissions from human activities over the past six decades, with regional differences. | Yes | / | I | Positive | Positive_correlation | human activities | increases in well-mixed greenhouse gases concentrations | null | since around 1750 | human activities | well-mixed greenhouse gases concentrations | null | null | GHG: greenhouse gas | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
827 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q101-2da3a440-4ee1-ec4f-b99f-cc456ee2f24e | 2.1.1 Observed Warming and its Causes | 2.1.1.b | 1 | Observed increases in well-mixed GHG concentrations since around 1750 are unequivocally caused by GHG emissions from human activities. Land and ocean sinks have taken up a near-constant proportion (globally about 56% per year) of CO2 emissions from human activities over the past six decades, with regional differences. | Yes | from | E | Positive | Positive_correlation | human activities | greenhouse gases emissions | null | null | human activities | greenhouse gases emissions | null | null | GHG = greenhouse gases | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
828 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q101-2da3a440-4ee1-ec4f-b99f-cc456ee2f24e | 2.1.1 Observed Warming and its Causes | 2.1.1.b | 1 | Observed increases in well-mixed GHG concentrations since around 1750 are unequivocally caused by GHG emissions from human activities. Land and ocean sinks have taken up a near-constant proportion (globally about 56% per year) of CO2 emissions from human activities over the past six decades, with regional differences. | Yes | from | E | Positive | Positive_correlation | human activities | carbon dioxide emissions | null | null | human activities | carbon dioxide emissions | null | null | CO2 = carbon dioxide | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
829 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q101-777c640c-4997-9e51-252c-d305174f36e5 | 2.1.1 Observed Warming and its Causes | 2.1.1.b | 4 | The net cooling effect which arises from anthropogenic aerosols peaked in the late 20th century. | Yes | arises from | E | Positive | Positive_correlation | anthropogenic aerosols | net cooling effect | null | null | anthropogenic aerosols | net cooling effect | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
830 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q101-777c640c-4997-9e51-252c-d305174f36e5 | 2.1.1 Observed Warming and its Causes | 2.1.1.b | 4 | The net cooling effect which arises from anthropogenic aerosols peaked in the late 20th century. | Yes | anthropogenic | I | Positive | Positive_correlation | humans | aerosols | null | null | human activities | aerosols | null | anthropogenic aerosols | null | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | Yes |
831 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q232-ed018ead-4e78-e511-d571-978a56763474 | 4.9 Integration of Near-Term Actions Across Sectors and Systems | 4.9.d | 1 | Mitigation and adaptation when implemented together, and combined with broader sustainable development objectives, would yield multiple benefits for human well-being as well as ecosystem and planetary health. | Yes | yield | E | Positive | Positive_correlation | mitigation | multiple benefits for human well-being | null | null | mitigation | benefits for human well-being | mitigation and adaptation when implemented together, and combined with broader sustainable development objectives | null | null | Yes | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
832 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q232-ed018ead-4e78-e511-d571-978a56763474 | 4.9 Integration of Near-Term Actions Across Sectors and Systems | 4.9.d | 1 | Mitigation and adaptation when implemented together, and combined with broader sustainable development objectives, would yield multiple benefits for human well-being as well as ecosystem and planetary health. | Yes | yield | E | Positive | Positive_correlation | mitigation | multiple benefits for ecosystem health | null | null | mitigation | benefits for ecosystem health | mitigation and adaptation when implemented together, and combined with broader sustainable development objectives | null | null | Yes | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
833 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q232-ed018ead-4e78-e511-d571-978a56763474 | 4.9 Integration of Near-Term Actions Across Sectors and Systems | 4.9.d | 1 | Mitigation and adaptation when implemented together, and combined with broader sustainable development objectives, would yield multiple benefits for human well-being as well as ecosystem and planetary health. | Yes | yield | E | Positive | Positive_correlation | mitigation | multiple benefits for planetary health | null | null | mitigation | benefits for planetary health | mitigation and adaptation when implemented together, and combined with broader sustainable development objectives | null | null | Yes | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
834 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q232-ed018ead-4e78-e511-d571-978a56763474 | 4.9 Integration of Near-Term Actions Across Sectors and Systems | 4.9.d | 1 | Mitigation and adaptation when implemented together, and combined with broader sustainable development objectives, would yield multiple benefits for human well-being as well as ecosystem and planetary health. | Yes | yield | E | Positive | Positive_correlation | adaptation | multiple benefits for human well-being | null | null | adaptation | benefits for human well-being | mitigation and adaptation when implemented together, and combined with broader sustainable development objectives | null | null | Yes | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
835 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q232-ed018ead-4e78-e511-d571-978a56763474 | 4.9 Integration of Near-Term Actions Across Sectors and Systems | 4.9.d | 1 | Mitigation and adaptation when implemented together, and combined with broader sustainable development objectives, would yield multiple benefits for human well-being as well as ecosystem and planetary health. | Yes | yield | E | Positive | Positive_correlation | adaptation | multiple benefits for ecosystem health | null | null | adaptation | benefits for ecosystem health | mitigation and adaptation when implemented together, and combined with broader sustainable development objectives | null | null | Yes | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
836 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q232-ed018ead-4e78-e511-d571-978a56763474 | 4.9 Integration of Near-Term Actions Across Sectors and Systems | 4.9.d | 1 | Mitigation and adaptation when implemented together, and combined with broader sustainable development objectives, would yield multiple benefits for human well-being as well as ecosystem and planetary health. | Yes | yield | E | Positive | Positive_correlation | adaptation | multiple benefits for planetary health | null | null | adaptation | benefits for planetary health | mitigation and adaptation when implemented together, and combined with broader sustainable development objectives | null | null | Yes | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
837 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q232-ed018ead-4e78-e511-d571-978a56763474 | 4.9 Integration of Near-Term Actions Across Sectors and Systems | 4.9.d | 1 | Mitigation and adaptation when implemented together, and combined with broader sustainable development objectives, would yield multiple benefits for human well-being as well as ecosystem and planetary health. | Yes | yield | E | Positive | Positive_correlation | Broader sustainable development objectives | multiple benefits for planetary health | null | null | sustainable development objectives | benefits for planetary health | mitigation and adaptation when implemented together, and combined with broader sustainable development objectives | null | null | Yes | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
838 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q232-ed018ead-4e78-e511-d571-978a56763474 | 4.9 Integration of Near-Term Actions Across Sectors and Systems | 4.9.d | 1 | Mitigation and adaptation when implemented together, and combined with broader sustainable development objectives, would yield multiple benefits for human well-being as well as ecosystem and planetary health. | Yes | yield | E | Positive | Positive_correlation | Broader sustainable development objectives | multiple benefits for human well-being | null | null | sustainable development objectives | benefits for human well-being | mitigation and adaptation when implemented together, and combined with broader sustainable development objectives | null | null | Yes | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
839 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q232-ed018ead-4e78-e511-d571-978a56763474 | 4.9 Integration of Near-Term Actions Across Sectors and Systems | 4.9.d | 1 | Mitigation and adaptation when implemented together, and combined with broader sustainable development objectives, would yield multiple benefits for human well-being as well as ecosystem and planetary health. | Yes | yield | E | Positive | Positive_correlation | Broader sustainable development objectives | multiple benefits for ecosystem health | null | null | sustainable development objectives | benefits for ecosystem health | mitigation and adaptation when implemented together, and combined with broader sustainable development objectives | null | null | Yes | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
840 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q232-ed018ead-4e78-e511-d571-978a56763474 | 4.9 Integration of Near-Term Actions Across Sectors and Systems | 4.9.d | 1 | Mitigation and adaptation when implemented together, and combined with broader sustainable development objectives, would yield multiple benefits for human well-being as well as ecosystem and planetary health. | Yes | yield | E | Positive | Positive_correlation | Mitigation and adaptation when implemented together, and combined with broader sustainable development objectives | multiple benefits for human well-being | null | null | mitigation and adaptation when implemented together, and combined with broader sustainable development objectives | benefits for human well-being | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
841 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q232-ed018ead-4e78-e511-d571-978a56763474 | 4.9 Integration of Near-Term Actions Across Sectors and Systems | 4.9.d | 1 | Mitigation and adaptation when implemented together, and combined with broader sustainable development objectives, would yield multiple benefits for human well-being as well as ecosystem and planetary health. | Yes | yield | E | Positive | Positive_correlation | Mitigation and adaptation when implemented together, and combined with broader sustainable development objectives | multiple benefits for ecosystem health | null | null | mitigation and adaptation when implemented together, and combined with broader sustainable development objectives | benefits for ecosystem health | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
842 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q232-ed018ead-4e78-e511-d571-978a56763474 | 4.9 Integration of Near-Term Actions Across Sectors and Systems | 4.9.d | 1 | Mitigation and adaptation when implemented together, and combined with broader sustainable development objectives, would yield multiple benefits for human well-being as well as ecosystem and planetary health. | Yes | yield | E | Positive | Positive_correlation | Mitigation and adaptation when implemented together, and combined with broader sustainable development objectives | multiple benefits for planetary health | null | null | mitigation and adaptation when implemented together, and combined with broader sustainable development objectives | benefits for planetary health | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
843 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff4 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | lead to | E | Positive | Positive_correlation | combined changes in Short-Lived Climate Forcers emissions | net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019 | null | In high and very high greenhouse gases emissions scenarios (SSP3-7.0 and SSP5-8.5) | combined changes in Short-Lived Climate Forcers emissions | net global warming | null | null | SLCF = Short-Lived Climate Forcers; GHG = greenhouse gases | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
844 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff4 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | lead to | E | Positive | Positive_correlation | changes in methane emissions | net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019 | null | In high and very high greenhouse gases emissions scenarios (SSP3-7.0 and SSP5-8.5) | changes in methane emissions | net global warming | combined changes in Short-Lived Climate Forcers emissions | null | SLCF = Short-Lived Climate Forcers; GHG = greenhouse gases; CH4 = methane | Yes | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
845 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff4 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | lead to | E | Positive | Positive_correlation | changes in aerosol emissions | net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019 | null | In high and very high greenhouse gases emissions scenarios (SSP3-7.0 and SSP5-8.5) | changes in aerosol emissions | net global warming | combined changes in Short-Lived Climate Forcers emissions | null | SLCF = Short-Lived Climate Forcers; GHG = greenhouse gases | Yes | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
846 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff4 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | lead to | E | Positive | Positive_correlation | changes in ozone precursors emissions | net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019 | null | In high and very high greenhouse gases emissions scenarios (SSP3-7.0 and SSP5-8.5) | changes in ozone precursors emissions | net global warming | combined changes in Short-Lived Climate Forcers emissions | null | SLCF = Short-Lived Climate Forcers; GHG = greenhouse gases | Yes | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
847 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff3 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | due to | E | Positive | Positive_correlation | increases in atmospheric concentration of methane | changes in short-lived climate forcers | null | null | atmospheric concentration of methane | changes in short-lived climate forcers | null | combined changes in Short-Lived Climate Forcers emissions | SLCF = Short-Lived Climate Forcers; CH4 = methane; GHG = greenhouse gases | Yes | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | No |
848 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff3 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | due to | E | Positive | Positive_correlation | increases in atmospheric concentration of tropospheric ozone | changes in short-lived climate forcers | null | null | atmospheric concentration of tropospheric ozone | changes in short-lived climate forcers | null | combined changes in Short-Lived Climate Forcers emissions | SLCF = Short-Lived Climate Forcers; GHG = greenhouse gases | Yes | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | No |
849 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff3 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | due to | E | Positive | Positive_correlation | increases in atmospheric concentration of hydrofluorocarbons | changes in short-lived climate forcers | null | null | atmospheric concentration of hydrofluorocarbons | changes in short-lived climate forcers | null | combined changes in Short-Lived Climate Forcers emissions | SLCF = Short-Lived Climate Forcers; GHG = greenhouse gases | Yes | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | No |
850 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff3 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | due to | E | Positive | Negative_correlation | reductions of cooling aerosols | changes in short-lived climate forcers | null | null | cooling aerosols | changes in short-lived climate forcers | null | combined changes in Short-Lived Climate Forcers emissions | SLCF = Short-Lived Climate Forcers; GHG = greenhouse gases | Yes | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | No |
851 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff3 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | due to | E | Positive | Positive_correlation | increases in atmospheric concentration of methane | net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019 | null | In high and very high greenhouse gases emissions scenarios (SSP3-7.0 and SSP5-8.5) | atmospheric concentration of methane | net global warming | null | null | CH4 = methane; GHG = greenhouse gases | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
852 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff2 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | due to | E | Positive | Positive_correlation | increases in atmospheric concentration of tropospheric ozone | net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019 | null | In high and very high greenhouse gases emissions scenarios (SSP3-7.0 and SSP5-8.5) | atmospheric concentration of tropospheric ozone | net global warming | null | null | GHG = greenhouse gases | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
853 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff1 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | due to | E | Positive | Positive_correlation | increases in atmospheric concentration of hydrofluorocarbons | net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019 | null | In high and very high greenhouse gases emissions scenarios (SSP3-7.0 and SSP5-8.5) | atmospheric concentration of hydrofluorocarbons | net global warming | null | null | GHG = greenhouse gases | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
854 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff0 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | due to | E | Positive | Negative_correlation | reductions of cooling aerosols | net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019 | when strong air pollution control is considered | In high and very high greenhouse gases emissions scenarios (SSP3-7.0 and SSP5-8.5) | cooling aerosols | net global warming | null | null | GHG = greenhouse gases | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
855 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff1 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | lead to | E | Positive | Positive_correlation | air pollution control policies | net cooling | null | In low and very low greenhouse gases emissions scenarios (SSP1- 1.9 and SSP1-2.6) | air pollution control policies | net cooling | null | null | GHG = greenhouse gases | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
856 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff2 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | lead to | E | Positive | Negative_correlation | reductions in methane | net cooling | null | In low and very low greenhouse gases emissions scenarios (SSP1- 1.9 and SSP1-2.6) | methane | net cooling | null | null | GHG = greenhouse gases; CH4 = methane | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
857 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff3 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | lead to | I | Positive | Negative_correlation | reductions of ozone precursors | net cooling | null | In low and very low greenhouse gases emissions scenarios (SSP1- 1.9 and SSP1-2.6) | ozone precursors | net cooling | null | null | GHG = greenhouse gases | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
858 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff4 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | lead to | E | Positive | Negative_correlation | reductions in anthropogenic cooling aerosols | net warming | null | In low and very low greenhouse gases emissions scenarios (SSP1- 1.9 and SSP1-2.6) | anthropogenic cooling aerosols | net warming | null | null | GHG = greenhouse gases | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
859 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff3 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | lead to | E | Positive | Negative_correlation | reductions of ozone precursors other than methane | net cooling | null | In low and very low greenhouse gases emissions scenarios (SSP1- 1.9 and SSP1-2.6) | ozone precursors other than methane | net cooling | null | null | GHG = greenhouse gases; CH4 = methane | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
860 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q152-1176a5e6-400e-2cc7-61dc-dcf5f9ae4ff4 | 3.1.1 Long-term Climate Change | 3.1.1.f | 3 | In high and very high GHG emissions scenarios (SSP3-7.0 and SSP5-8.5), combined changes in SLCF emissions, such as CH4, aerosol and ozone precursors, lead to a net global warming by 2100 of likely 0.4°C–0.9°C relative to 2019. This is due to projected increases in atmospheric concentration of CH4, tropospheric ozone, h... | Yes | anthropogenic | I | Positive | Positive_correlation | humans | cooling aerosols | null | null | human activities | cooling aerosols | null | anthropogenic cooling aerosols | GHG = greenhouse gases | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | Yes |
861 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q103-e7838c5b-4d91-5c1a-36d5-bea860d55f4c | 2.1.1 Observed Warming and its Causes | 2.1.1.g | 1 | Regional contributions to global human-caused GHG emissions continue to differ widely. Historical contributions of CO2 emissions vary substantially across regions in terms of total magnitude, but also in terms of contributions to CO2-FFI (1650 ± 73 GtCO2-eq) and net CO2-LULUCF (760 ± 220 GtCO2-eq) emissions (Figure 2.2... | Yes | caused | E | Positive | Positive_correlation | humans | greenhouse gases emissions | null | null | human activities | greenhouse gases emissions | null | human-caused greenhouse gases emissions | GHG = greenhouse gases | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | Yes |
862 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q241-9acd53e9-4c97-c7be-aa88-7cd85a3a3eb0 | 2.1.1 Observed Warming and its Causes | 2.1.1.g | 1 | Regional contributions to global human-caused GHG emissions continue to differ widely. Historical contributions of CO2 emissions vary substantially across regions in terms of total magnitude, but also in terms of contributions to CO2-FFI (1650 ± 73 GtCO2-eq) and net CO2-LULUCF (760 ± 220 GtCO2-eq) emissions (Figure 2.2... | Yes | CO2-FFI | I | Positive | Positive_correlation | fossil fuel combustion | carbon dioxide emission | null | null | fossil fuel combustion | carbon dioxide emission | null | CO2-FFI | CO2 = carbon dioxide | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | Yes |
863 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q241-9acd53e9-4c97-c7be-aa88-7cd85a3a3eb0 | 2.1.1 Observed Warming and its Causes | 2.1.1.g | 1 | Regional contributions to global human-caused GHG emissions continue to differ widely. Historical contributions of CO2 emissions vary substantially across regions in terms of total magnitude, but also in terms of contributions to CO2-FFI (1650 ± 73 GtCO2-eq) and net CO2-LULUCF (760 ± 220 GtCO2-eq) emissions (Figure 2.2... | Yes | CO2-FFI | I | Positive | Positive_correlation | industrial processes | carbon dioxide emission | null | null | industrial processes | carbon dioxide emission | null | CO2-FFI | CO2 = carbon dioxide | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | Yes |
864 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q241-9acd53e9-4c97-c7be-aa88-7cd85a3a3eb0 | 2.1.1 Observed Warming and its Causes | 2.1.1.g | 1 | Regional contributions to global human-caused GHG emissions continue to differ widely. Historical contributions of CO2 emissions vary substantially across regions in terms of total magnitude, but also in terms of contributions to CO2-FFI (1650 ± 73 GtCO2-eq) and net CO2-LULUCF (760 ± 220 GtCO2-eq) emissions (Figure 2.2... | Yes | CO2-LULUCF | I | Positive | Positive_correlation | land use sector | carbon dioxide emission | null | null | land use sector | carbon dioxide emission | null | CO2-LULUCF | CO2 = carbon dioxide | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | Yes |
865 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q241-9acd53e9-4c97-c7be-aa88-7cd85a3a3eb0 | 2.1.1 Observed Warming and its Causes | 2.1.1.g | 1 | Regional contributions to global human-caused GHG emissions continue to differ widely. Historical contributions of CO2 emissions vary substantially across regions in terms of total magnitude, but also in terms of contributions to CO2-FFI (1650 ± 73 GtCO2-eq) and net CO2-LULUCF (760 ± 220 GtCO2-eq) emissions (Figure 2.2... | Yes | CO2-LULUCF | I | Positive | Positive_correlation | land-use change sector | carbon dioxide emission | null | null | land-use change sector | carbon dioxide emission | null | CO2-LULUCF | CO2 = carbon dioxide | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | Yes |
866 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q241-9acd53e9-4c97-c7be-aa88-7cd85a3a3eb0 | 2.1.1 Observed Warming and its Causes | 2.1.1.g | 1 | Regional contributions to global human-caused GHG emissions continue to differ widely. Historical contributions of CO2 emissions vary substantially across regions in terms of total magnitude, but also in terms of contributions to CO2-FFI (1650 ± 73 GtCO2-eq) and net CO2-LULUCF (760 ± 220 GtCO2-eq) emissions (Figure 2.2... | Yes | CO2-LULUCF | I | Positive | Positive_correlation | forestry sector | carbon dioxide emission | null | null | forestry sector | carbon dioxide emission | null | CO2-LULUCF | CO2 = carbon dioxide | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | Yes |
867 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q241-9acd53e9-4c97-c7be-aa88-7cd85a3a3eb0 | 2.1.1 Observed Warming and its Causes | 2.1.1.g | 1 | Regional contributions to global human-caused GHG emissions continue to differ widely. Historical contributions of CO2 emissions vary substantially across regions in terms of total magnitude, but also in terms of contributions to CO2-FFI (1650 ± 73 GtCO2-eq) and net CO2-LULUCF (760 ± 220 GtCO2-eq) emissions (Figure 2.2... | Yes | anthropogenic | I | Positive | Positive_correlation | humans | greenhouse gases emissions | null | null | human activities | greenhouse gases emissions | null | anthropogenic greenhouse gases emissions | CO2 = carbon dioxide | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | Yes |
868 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q114-fe297ae8-43e1-be2b-6095-956f085d00d3 | 2.1.2 Observed Climate System Changes and Impacts to Date | 2.1.2.l | 7 | Between 2010 and 2020, human mortality from floods, droughts and storms was 15 times higher in highly vulnerable regions, compared to regions with very low vulnerability. | Yes | from | E | Positive | Positive_correlation | Floods | Human mortality | null | null | floods | human mortality | null | human mortality from floods | null | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | Yes |
869 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q114-fe297ae8-43e1-be2b-6095-956f085d00d3 | 2.1.2 Observed Climate System Changes and Impacts to Date | 2.1.2.l | 7 | Between 2010 and 2020, human mortality from floods, droughts and storms was 15 times higher in highly vulnerable regions, compared to regions with very low vulnerability. | Yes | from | E | Positive | Positive_correlation | Droughts | Human mortality | null | null | droughts | human mortality | null | human mortality from droughts | null | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | Yes |
870 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q114-fe297ae8-43e1-be2b-6095-956f085d00d3 | 2.1.2 Observed Climate System Changes and Impacts to Date | 2.1.2.l | 7 | Between 2010 and 2020, human mortality from floods, droughts and storms was 15 times higher in highly vulnerable regions, compared to regions with very low vulnerability. | Yes | from | E | Positive | Positive_correlation | Storms | Human mortality | null | null | storms | human mortality | null | human mortality from storms | null | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | Yes |
871 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q114-fe297ae8-43e1-be2b-6095-956f085d00d6 | 2.1.2 Observed Climate System Changes and Impacts to Date | 2.1.2.l | 7 | Between 2010 and 2020, human mortality from floods, droughts and storms was 15 times higher in highly vulnerable regions, compared to regions with very low vulnerability. | Yes | / | I | Positive | Positive_correlation | higher vulnerability of a region to climatic hazards | higher human mortality from floods | null | null | vulnerability to climatic hazards | human mortality from floods | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
872 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q114-fe297ae8-43e1-be2b-6095-956f085d00d7 | 2.1.2 Observed Climate System Changes and Impacts to Date | 2.1.2.l | 7 | Between 2010 and 2020, human mortality from floods, droughts and storms was 15 times higher in highly vulnerable regions, compared to regions with very low vulnerability. | Yes | / | I | Positive | Positive_correlation | higher vulnerability of a region to climatic hazards | higher human mortality from droughts | null | null | vulnerability to climatic hazards | human mortality from droughts | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
873 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q114-fe297ae8-43e1-be2b-6095-956f085d00d8 | 2.1.2 Observed Climate System Changes and Impacts to Date | 2.1.2.l | 7 | Between 2010 and 2020, human mortality from floods, droughts and storms was 15 times higher in highly vulnerable regions, compared to regions with very low vulnerability. | Yes | / | I | Positive | Positive_correlation | higher vulnerability of a region to climatic hazards | higher human mortality from storms | null | null | vulnerability to climatic hazards | human mortality from storms | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
874 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5dff62ac-461f-0bc7-a1fc-245302cd5afb | 2.1.1 Observed Warming and its Causes | null | 1 | Human activities, principally through emissions of greenhouse gases, have unequivocally caused global warming, with global surface temperature reaching 1.1°C above 1850–1900 in 2011–2020. Global greenhouse gas emissions have continued to increase over 2010–2019, with unequal historical and ongoing contributions arising... | Yes | through | E | Positive | Positive_correlation | human activities | emissions of greenhouse gases | null | null | human activities | emissions of greenhouse gases | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
875 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5dff62ac-461f-0bc7-a1fc-245302cd5afb | 2.1.1 Observed Warming and its Causes | null | 1 | Human activities, principally through emissions of greenhouse gases, have unequivocally caused global warming, with global surface temperature reaching 1.1°C above 1850–1900 in 2011–2020. Global greenhouse gas emissions have continued to increase over 2010–2019, with unequal historical and ongoing contributions arising... | Yes | have unequivocally caused | E | Positive | Positive_correlation | human activities | global warming | null | null | human activities | global warming | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
876 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5dff62ac-461f-0bc7-a1fc-245302cd5afb | 2.1.1 Observed Warming and its Causes | null | 1 | Human activities, principally through emissions of greenhouse gases, have unequivocally caused global warming, with global surface temperature reaching 1.1°C above 1850–1900 in 2011–2020. Global greenhouse gas emissions have continued to increase over 2010–2019, with unequal historical and ongoing contributions arising... | Yes | have unequivocally caused | E | Positive | Positive_correlation | emissions of greenhouse gases | global warming | null | null | emissions of greenhouse gases | global warming | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
877 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5dff62ac-461f-0bc7-a1fc-245302cd5afb | 2.1.1 Observed Warming and its Causes | null | 1 | Human activities, principally through emissions of greenhouse gases, have unequivocally caused global warming, with global surface temperature reaching 1.1°C above 1850–1900 in 2011–2020. Global greenhouse gas emissions have continued to increase over 2010–2019, with unequal historical and ongoing contributions arising... | Yes | caused | E | Positive | Positive_correlation | human activities | global surface temperatures reaching 1.1°C above 1850–1900 | null | in 2011-2020 | human activities | global surface temperatures | null | global warming | null | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | No |
878 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5dff62ac-461f-0bc7-a1fc-245302cd5afb | 2.1.1 Observed Warming and its Causes | null | 1 | Human activities, principally through emissions of greenhouse gases, have unequivocally caused global warming, with global surface temperature reaching 1.1°C above 1850–1900 in 2011–2020. Global greenhouse gas emissions have continued to increase over 2010–2019, with unequal historical and ongoing contributions arising... | Yes | / | I | Positive | Positive_correlation | Human activities | continued increase in global greenhouse gas emissions | null | over 2010–2019 | human activities | global greenhouse gas emissions | null | emissions of greenhouse gases | null | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | No |
879 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5dff62ac-461f-0bc7-a1fc-245302cd5afb | 2.1.1 Observed Warming and its Causes | null | 1 | Human activities, principally through emissions of greenhouse gases, have unequivocally caused global warming, with global surface temperature reaching 1.1°C above 1850–1900 in 2011–2020. Global greenhouse gas emissions have continued to increase over 2010–2019, with unequal historical and ongoing contributions arising... | Yes | unequal historical and ongoing contributions arising from | E | Positive | Positive_correlation | unsustainable energy use | continued increase in global greenhouse gas emissions | null | over 2010–2019 | unsustainable energy use | global greenhouse gas emissions | human activities | emissions of greenhouse gases | null | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | No |
880 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5dff62ac-461f-0bc7-a1fc-245302cd5afb | 2.1.1 Observed Warming and its Causes | null | 1 | Human activities, principally through emissions of greenhouse gases, have unequivocally caused global warming, with global surface temperature reaching 1.1°C above 1850–1900 in 2011–2020. Global greenhouse gas emissions have continued to increase over 2010–2019, with unequal historical and ongoing contributions arising... | Yes | unequal historical and ongoing contributions arising from | E | Positive | Positive_correlation | unsustainable land use | continued increase in global greenhouse gas emissions | null | over 2010–2019 | unsustainable land use | global greenhouse gas emissions | human activities | emissions of greenhouse gases | null | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | No |
881 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5dff62ac-461f-0bc7-a1fc-245302cd5afb | 2.1.1 Observed Warming and its Causes | null | 1 | Human activities, principally through emissions of greenhouse gases, have unequivocally caused global warming, with global surface temperature reaching 1.1°C above 1850–1900 in 2011–2020. Global greenhouse gas emissions have continued to increase over 2010–2019, with unequal historical and ongoing contributions arising... | Yes | unequal historical and ongoing contributions arising from | E | Positive | Positive_correlation | unsustainable land-use change | continued increase in global greenhouse gas emissions | null | over 2010–2019 | unsustainable land-use change | global greenhouse gas emissions | human activities | emissions of greenhouse gases | null | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | No |
882 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5dff62ac-461f-0bc7-a1fc-245302cd5afb | 2.1.1 Observed Warming and its Causes | null | 1 | Human activities, principally through emissions of greenhouse gases, have unequivocally caused global warming, with global surface temperature reaching 1.1°C above 1850–1900 in 2011–2020. Global greenhouse gas emissions have continued to increase over 2010–2019, with unequal historical and ongoing contributions arising... | Yes | unequal historical and ongoing contributions arising from | E | Positive | Positive_correlation | unsustainable lifestyles | continued increase in global greenhouse gas emissions | null | over 2010–2019 | unsustainable lifestyles | global greenhouse gas emissions | human activities | emissions of greenhouse gases | null | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | No |
883 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5dff62ac-461f-0bc7-a1fc-245302cd5afb | 2.1.1 Observed Warming and its Causes | null | 1 | Human activities, principally through emissions of greenhouse gases, have unequivocally caused global warming, with global surface temperature reaching 1.1°C above 1850–1900 in 2011–2020. Global greenhouse gas emissions have continued to increase over 2010–2019, with unequal historical and ongoing contributions arising... | Yes | unequal historical and ongoing contributions arising from | E | Positive | Positive_correlation | unsustainable patterns of consumption | continued increase in global greenhouse gas emissions | null | over 2010–2019 | unsustainable patterns of consumption | global greenhouse gas emissions | human activities | emissions of greenhouse gases | null | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | No |
884 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5dff62ac-461f-0bc7-a1fc-245302cd5afb | 2.1.1 Observed Warming and its Causes | null | 1 | Human activities, principally through emissions of greenhouse gases, have unequivocally caused global warming, with global surface temperature reaching 1.1°C above 1850–1900 in 2011–2020. Global greenhouse gas emissions have continued to increase over 2010–2019, with unequal historical and ongoing contributions arising... | Yes | unequal historical and ongoing contributions arising from | E | Positive | Positive_correlation | unsustainable patterns of production | continued increase in global greenhouse gas emissions | null | over 2010–2019 | unsustainable patterns of production | global greenhouse gas emissions | human activities | emissions of greenhouse gases | null | No | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | No |
885 | https://kg-ipclimatec-reports.wikibase.cloud/entity/statement/Q67-5de54124-4a60-67d4-28d2-0f7cde9fa3ee | 2.1.1 Observed Warming and its Causes | null | 3 | Vulnerable communities who have historically contributed the least to current climate change are disproportionately affected. | No | null | null | null | null | null | null | null | null | null | null | null | null | null | null | https://kg-ipclimatec-reports.wikibase.cloud/entity/Q2 | high confidence | null |
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