Strategies and mechanisms for mainstreaming climate change into agriculture and irrigation sector reforms

Global warming is unequivocal, and since 1950s, many of the observed changes are unprecedented over decades to millennia. The atmosphere has warmed (0.85oC over the period 1883 to 2012). Glaciers have continued to shrink almost worldwide. The amounts of snow and ice have diminished. The Greenland an...

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Main Author: Rana, Abdul Wajid
Format: Report
Language:unknown
Subjects:
Online Access:https://www.ifpri.org/cdmref/p15738coll2/id/133442/filename/133653.pdf
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spelling ftrepec:oai:RePEc:fpr:pacerp:1 2024-04-14T08:01:48+00:00 Strategies and mechanisms for mainstreaming climate change into agriculture and irrigation sector reforms Rana, Abdul Wajid https://www.ifpri.org/cdmref/p15738coll2/id/133442/filename/133653.pdf unknown https://www.ifpri.org/cdmref/p15738coll2/id/133442/filename/133653.pdf preprint ftrepec 2024-03-19T10:33:53Z Global warming is unequivocal, and since 1950s, many of the observed changes are unprecedented over decades to millennia. The atmosphere has warmed (0.85oC over the period 1883 to 2012). Glaciers have continued to shrink almost worldwide. The amounts of snow and ice have diminished. The Greenland and Antarctic ice sheets have been losing mass. The sea level has risen and on a global scale, the ocean warming is largest near the surface, and the upper 75 m warmed by 0.11°C per decade over the period 1971 to 2010. The increase in greenhouse gas (GHG) emissions, driven largely by economic and population growth, together with other anthropological drivers have caused changes in climate system. Continued emission of greenhouse gases is expected to cause further warming and changes in the climate system increasing the possibilities of severe and irreversible impacts for people and ecosystem. Surface temperature is projected to rise over the 21st century (0.3 to 1.7oC) and it is likely that heat waves will occur more frequently and last longer. The global ocean will continue to warm during the 21st century, with the strongest warming projected for the surface in tropical and Northern Hemisphere subtropical regions. The global glacier volume excluding glaciers on the periphery of Antarctica (and excluding the Greenland and Antarctic ice sheets) is projected to decrease by 15 to 55%.1 Therefore, limiting climate change would need substantial and sustained reduction in greenhouse gas emissions through adaptation and mitigation strategies. These include innovation and investment in environmentally sound technologies and infrastructure, sustainable livelihoods and behavioural and lifestyles choices as well as effective institutions and governance. PAKISTAN, SOUTH ASIA, ASIA, climate change, irrigation, agriculture, water, global warming, greenhouse gases Report Antarc* Antarctic Antarctica glacier Greenland RePEc (Research Papers in Economics) Antarctic Greenland
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description Global warming is unequivocal, and since 1950s, many of the observed changes are unprecedented over decades to millennia. The atmosphere has warmed (0.85oC over the period 1883 to 2012). Glaciers have continued to shrink almost worldwide. The amounts of snow and ice have diminished. The Greenland and Antarctic ice sheets have been losing mass. The sea level has risen and on a global scale, the ocean warming is largest near the surface, and the upper 75 m warmed by 0.11°C per decade over the period 1971 to 2010. The increase in greenhouse gas (GHG) emissions, driven largely by economic and population growth, together with other anthropological drivers have caused changes in climate system. Continued emission of greenhouse gases is expected to cause further warming and changes in the climate system increasing the possibilities of severe and irreversible impacts for people and ecosystem. Surface temperature is projected to rise over the 21st century (0.3 to 1.7oC) and it is likely that heat waves will occur more frequently and last longer. The global ocean will continue to warm during the 21st century, with the strongest warming projected for the surface in tropical and Northern Hemisphere subtropical regions. The global glacier volume excluding glaciers on the periphery of Antarctica (and excluding the Greenland and Antarctic ice sheets) is projected to decrease by 15 to 55%.1 Therefore, limiting climate change would need substantial and sustained reduction in greenhouse gas emissions through adaptation and mitigation strategies. These include innovation and investment in environmentally sound technologies and infrastructure, sustainable livelihoods and behavioural and lifestyles choices as well as effective institutions and governance. PAKISTAN, SOUTH ASIA, ASIA, climate change, irrigation, agriculture, water, global warming, greenhouse gases
format Report
author Rana, Abdul Wajid
spellingShingle Rana, Abdul Wajid
Strategies and mechanisms for mainstreaming climate change into agriculture and irrigation sector reforms
author_facet Rana, Abdul Wajid
author_sort Rana, Abdul Wajid
title Strategies and mechanisms for mainstreaming climate change into agriculture and irrigation sector reforms
title_short Strategies and mechanisms for mainstreaming climate change into agriculture and irrigation sector reforms
title_full Strategies and mechanisms for mainstreaming climate change into agriculture and irrigation sector reforms
title_fullStr Strategies and mechanisms for mainstreaming climate change into agriculture and irrigation sector reforms
title_full_unstemmed Strategies and mechanisms for mainstreaming climate change into agriculture and irrigation sector reforms
title_sort strategies and mechanisms for mainstreaming climate change into agriculture and irrigation sector reforms
url https://www.ifpri.org/cdmref/p15738coll2/id/133442/filename/133653.pdf
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