The influence of dynamic vegetation on the present-day simulation and future projections of the South Asian summer monsoon in the HadGEM2 family

Various studies have shown the importance of Earth System feedbacks in the climate system and the necessity of including these in models used for making climate change projections. The HadGEM2 family of Met Office Unified Model configurations combines model components which facilitate the representa...

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Published in:Earth System Dynamics
Main Authors: Martin, G. M., Levine, R. C.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/esd-3-245-2012
https://esd.copernicus.org/articles/3/245/2012/
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spelling ftcopernicus:oai:publications.copernicus.org:esd16517 2023-05-15T18:18:36+02:00 The influence of dynamic vegetation on the present-day simulation and future projections of the South Asian summer monsoon in the HadGEM2 family Martin, G. M. Levine, R. C. 2018-09-27 application/pdf https://doi.org/10.5194/esd-3-245-2012 https://esd.copernicus.org/articles/3/245/2012/ eng eng doi:10.5194/esd-3-245-2012 https://esd.copernicus.org/articles/3/245/2012/ eISSN: 2190-4987 Text 2018 ftcopernicus https://doi.org/10.5194/esd-3-245-2012 2020-07-20T16:25:38Z Various studies have shown the importance of Earth System feedbacks in the climate system and the necessity of including these in models used for making climate change projections. The HadGEM2 family of Met Office Unified Model configurations combines model components which facilitate the representation of many different processes within the climate system, including atmosphere, ocean and sea ice, and Earth System components including the terrestrial and oceanic carbon cycle and tropospheric chemistry. We examine the climatology of the Asian summer monsoon in present-day simulations and in idealised climate change experiments. Members of the HadGEM2 family are used, with a common physical framework (one of which includes tropospheric chemistry and an interactive terrestrial and oceanic carbon cycle), to investigate whether such components affect the way in which the monsoon changes. We focus particularly on the role of interactive vegetation in the simulations from these model configurations. Using an atmosphere-only HadGEM2 configuration, we investigate how the changes in land cover which result from the interaction between the dynamic vegetation and the model systematic rainfall biases affect the Asian summer monsoon, both in the present-day and in future climate projections. We demonstrate that the response of the dynamic vegetation to biases in regional climate, such as lack of rainfall over tropical dust-producing regions, can affect both the present-day simulation and the response to climate change forcing scenarios. Text Sea ice Copernicus Publications: E-Journals Earth System Dynamics 3 2 245 261
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Various studies have shown the importance of Earth System feedbacks in the climate system and the necessity of including these in models used for making climate change projections. The HadGEM2 family of Met Office Unified Model configurations combines model components which facilitate the representation of many different processes within the climate system, including atmosphere, ocean and sea ice, and Earth System components including the terrestrial and oceanic carbon cycle and tropospheric chemistry. We examine the climatology of the Asian summer monsoon in present-day simulations and in idealised climate change experiments. Members of the HadGEM2 family are used, with a common physical framework (one of which includes tropospheric chemistry and an interactive terrestrial and oceanic carbon cycle), to investigate whether such components affect the way in which the monsoon changes. We focus particularly on the role of interactive vegetation in the simulations from these model configurations. Using an atmosphere-only HadGEM2 configuration, we investigate how the changes in land cover which result from the interaction between the dynamic vegetation and the model systematic rainfall biases affect the Asian summer monsoon, both in the present-day and in future climate projections. We demonstrate that the response of the dynamic vegetation to biases in regional climate, such as lack of rainfall over tropical dust-producing regions, can affect both the present-day simulation and the response to climate change forcing scenarios.
format Text
author Martin, G. M.
Levine, R. C.
spellingShingle Martin, G. M.
Levine, R. C.
The influence of dynamic vegetation on the present-day simulation and future projections of the South Asian summer monsoon in the HadGEM2 family
author_facet Martin, G. M.
Levine, R. C.
author_sort Martin, G. M.
title The influence of dynamic vegetation on the present-day simulation and future projections of the South Asian summer monsoon in the HadGEM2 family
title_short The influence of dynamic vegetation on the present-day simulation and future projections of the South Asian summer monsoon in the HadGEM2 family
title_full The influence of dynamic vegetation on the present-day simulation and future projections of the South Asian summer monsoon in the HadGEM2 family
title_fullStr The influence of dynamic vegetation on the present-day simulation and future projections of the South Asian summer monsoon in the HadGEM2 family
title_full_unstemmed The influence of dynamic vegetation on the present-day simulation and future projections of the South Asian summer monsoon in the HadGEM2 family
title_sort influence of dynamic vegetation on the present-day simulation and future projections of the south asian summer monsoon in the hadgem2 family
publishDate 2018
url https://doi.org/10.5194/esd-3-245-2012
https://esd.copernicus.org/articles/3/245/2012/
genre Sea ice
genre_facet Sea ice
op_source eISSN: 2190-4987
op_relation doi:10.5194/esd-3-245-2012
https://esd.copernicus.org/articles/3/245/2012/
op_doi https://doi.org/10.5194/esd-3-245-2012
container_title Earth System Dynamics
container_volume 3
container_issue 2
container_start_page 245
op_container_end_page 261
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