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        <dc:title>Integrated Assessments of the Impact of Climate Change on Agriculture: An Overview of AgMIP Regional Research in South Asia</dc:title>
        <dc:creator>McDermid, S P</dc:creator>
        <dc:creator>Dileepkumar, G</dc:creator>
        <dc:creator>Kadiyala, M D M</dc:creator>
        <dc:creator>Nedumaran, S</dc:creator>
        <dc:creator>Singh, P</dc:creator>
        <dc:creator>Srinivasa, Chukka</dc:creator>
        <dc:creator>Gangwar, B.</dc:creator>
        <dc:creator>Subash, N.</dc:creator>
        <dc:creator>Ahmad, Ashfaq</dc:creator>
        <dc:creator>Zubair, Lareef</dc:creator>
        <dc:creator>Nissanka, S. P.</dc:creator>
        <dc:subject>Agriculture</dc:subject>
        <dc:subject>South Asia</dc:subject>
        <dc:subject>Climate Change</dc:subject>
        <dc:description>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.</dc:description>
        <dc:publisher>Imperial College Press</dc:publisher>
        <dc:contributor>Rosenzweig, C</dc:contributor>
        <dc:contributor>Hillel, D</dc:contributor>
        <dc:date>2015-04</dc:date>
        <dc:type>Book Section</dc:type>
        <dc:type>PeerReviewed</dc:type>
        <dc:format>application/pdf</dc:format>
        <dc:language>en</dc:language>
        <dc:identifier>http://oar.icrisat.org/10749/1/9781783265640_0018.pdf</dc:identifier>
        <dc:identifier>  McDermid, S P and Dileepkumar, G and Kadiyala, M D M and Nedumaran, S and Singh, P and Srinivasa, Chukka and Gangwar, B. and Subash, N. and Ahmad, Ashfaq and Zubair, Lareef and Nissanka, S. P.  (2015) Integrated Assessments of the Impact of Climate Change on Agriculture: An Overview of AgMIP Regional Research in South Asia.   In:  Handbook of Climate Change and Agroecosystems: The Agricultural Model Intercomparison and Improvement Project (AgMIP) Integrated Crop and Economic Assessments, Part 2.   ICP Series on Climate Change Impacts, Adaptation, and Mitigation — Vol. 3 .  Imperial College Press, London, pp. 201-217.  ISBN 978-1-78326-567-1     </dc:identifier>
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