Global Meteorological Drought: A Synthesis of Current Understanding with a Focus on SST Drivers of Precipitation Deficits
Author(s) -
Siegfried D. Schubert,
Ronald E. Stewart,
Hailan Wang,
Mathew Barlow,
Ernesto Hugo Berbery,
Wenju Cai,
Martin P. Hoerling,
Krishna Kumar Kanikicharla,
Randal D. Koster,
Bradfield Lyon,
Annarita Mariotti,
Carlos R. Mechoso,
Omar V. Müller,
Belén RodríguezFonseca,
Richard Seager,
Sonia I. Seneviratne,
Lixia Zhang,
Tianjun Zhou
Publication year - 2016
Publication title -
journal of climate
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 3.315
H-Index - 287
eISSN - 1520-0442
pISSN - 0894-8755
DOI - 10.1175/jcli-d-15-0452.1
Subject(s) - climatology , sea surface temperature , precipitation , environmental science , predictability , climate model , climate change , geography , oceanography , geology , meteorology , physics , quantum mechanics
Drought affects virtually every region of the world, and potential shifts in its character in a changing climate are a major concern. This article presents a synthesis of current understanding of meteorological drought, with a focus on the large-scale controls on precipitation afforded by sea surface temperature (SST) anomalies, land surface feedbacks, and radiative forcings. The synthesis is primarily based on regionally focused articles submitted to the Global Drought Information System (GDIS) collection together with new results from a suite of atmospheric general circulation model experiments intended to integrate those studies into a coherent view of drought worldwide. On interannual time scales, the preeminence of ENSO as a driver of meteorological drought throughout much of the Americas, eastern Asia, Australia, and the Maritime Continent is now well established, whereas in other regions (e.g., Europe, Africa, and India), the response to ENSO is more ephemeral or nonexistent. Northern Eurasia, central Europe, and central and eastern Canada stand out as regions with few SST-forced impacts on precipitation on interannual time scales. Decadal changes in SST appear to be a major factor in the occurrence of long-term drought, as highlighted by apparent impacts on precipitation of the late 1990s “climate shifts” in the Pacific and Atlantic SST. Key remaining research challenges include (i) better quantification of unforced and forced atmospheric variability as well as land–atmosphere feedbacks, (ii) better understanding of the physical basis for the leading modes of climate variability and their predictability, and (iii) quantification of the relative contributions of internal decadal SST variability and forced climate change to long-term drought.The various contributions to this\udpaper were made possible by the support of the host\udorganizations of the coauthors, as noted in the acknowledgments\udof the contributing Global Drought\udInformation System (GDIS) special collection papers.\udThe GDIS effort is sponsored and supported by\udthe World Climate Research Programme (WCRP:\udCLIVAR andGEWEX) and various partner organizations including the National Oceanic and Atmospheric Administration\ud(NOAA), the National Aeronautics and\udSpace Administration (NASA), the National Integrated\udDrought Information System (NIDIS), the World Meteorological\udOrganization (WMO), the U.S. CLIVAR\udprogram, the Group on Earth Observations (GEO), the\udEuropean Commission JointResearch Centre (JRC), the\udNational Science Foundation (NSF), and the European\udSpace Agency (ESA)–European Space Research Institute\ud(ESRIN). Support for the overall development of\udthis synthesis article was provided by NASA’sModeling,\udAnalysis and Prediction Program. The GLDAS-2 data\udused in this study were acquired as part of the mission of\udNASA’s Earth Science Division and archived and distributed\udby the Goddard Earth Sciences (GES) Data and\udInformation Services Center (DISC).Peer reviewe
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