<mets:mets OBJID="eprint_10749" LABEL="Eprints Item" xsi:schemaLocation="http://www.loc.gov/METS/ http://www.loc.gov/standards/mets/mets.xsd http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-3.xsd" xmlns:mets="http://www.loc.gov/METS/" xmlns:mods="http://www.loc.gov/mods/v3" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance"><mets:metsHdr CREATEDATE="2023-07-04T22:51:20Z"><mets:agent ROLE="CUSTODIAN" TYPE="ORGANIZATION"><mets:name>OAR@ICRISAT</mets:name></mets:agent></mets:metsHdr><mets:dmdSec ID="DMD_eprint_10749_mods"><mets:mdWrap MDTYPE="MODS"><mets:xmlData><mods:titleInfo><mods:title>Integrated Assessments of the Impact of Climate Change on Agriculture: An Overview of AgMIP Regional Research in South Asia</mods:title></mods:titleInfo><mods:name type="personal"><mods:namePart type="given">S P</mods:namePart><mods:namePart type="family">McDermid</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">G</mods:namePart><mods:namePart type="family">Dileepkumar</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">M D M</mods:namePart><mods:namePart type="family">Kadiyala</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">S</mods:namePart><mods:namePart type="family">Nedumaran</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">P</mods:namePart><mods:namePart type="family">Singh</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">Chukka</mods:namePart><mods:namePart type="family">Srinivasa</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">B.</mods:namePart><mods:namePart type="family">Gangwar</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">N.</mods:namePart><mods:namePart type="family">Subash</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">Ashfaq</mods:namePart><mods:namePart type="family">Ahmad</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">Lareef</mods:namePart><mods:namePart type="family">Zubair</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">S. P.</mods:namePart><mods:namePart type="family">Nissanka</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:abstract>South Asia encompasses a wide and highly varied geographic region, and includes&#13;
climate zones ranging from the mountainous Himalayan territory to the tropical lowland&#13;
and coastal zones along alluvial floodplains. The region’s climate is dominated&#13;
by a monsoonal circulation that heralds the arrival of seasonal rainfall, upon which&#13;
much of the regional agriculture relies (Mall et al., 2006). The spatial and temporal&#13;
distribution of this rainfall is, however, not uniform over the region. Northern&#13;
South Asia, central India, and the west coast receive much of their rainfall during&#13;
the southwest monsoon season, between June and September. These rains partly&#13;
result from the moisture transport accompanying the monsoonal winds, which move&#13;
in the southwesterly direction from the equatorial Indian Ocean. Regions further&#13;
south, such as south/southeast India and Sri Lanka, may receive rains both from the&#13;
southwest monsoon, and also during the northeast monsoon season between October&#13;
and December (with northeasterly monsoonal wind flow and moisture flux),&#13;
which results in a bi- or multi-modal rainfall distribution. In addition, rainfall across&#13;
South Asia displays a large amount of intraseasonal and interannual variability&#13;
(Fig. 1). Interannual variability is influenced by many drivers, both natural (e.g., El&#13;
Ni˜no Southern Oscillation; ENSO) and man-made (e.g., rising temperatures due to&#13;
increasing greenhouse gas concentrations), and it is challenging to obtaining accurate&#13;
time-series of annual rainfall, even amongst various observed data products,&#13;
which display inconsistencies amongst themselves (exemplified in Fig. 1). These&#13;
climatic and rainfall variations can further complicate South Asia’s agricultural and&#13;
water management.</mods:abstract><mods:classification authority="lcc">Agriculture</mods:classification><mods:classification authority="lcc">South Asia</mods:classification><mods:classification authority="lcc">Climate Change</mods:classification><mods:originInfo><mods:dateIssued encoding="iso8061">2015-04</mods:dateIssued></mods:originInfo><mods:originInfo><mods:publisher>Imperial College Press</mods:publisher></mods:originInfo><mods:genre>Book Section</mods:genre></mets:xmlData></mets:mdWrap></mets:dmdSec><mets:amdSec ID="TMD_eprint_10749"><mets:rightsMD ID="rights_eprint_10749_mods"><mets:mdWrap MDTYPE="MODS"><mets:xmlData><mods:useAndReproduction>
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