DOI: 10.1175/JCLI-D-16-0156.1
Scopus记录号: 2-s2.0-85014057168
论文题名: Role of oceanic and land moisture sources and transport in the seasonal and interannual variability of summer monsoon in India
作者: Pathak A. ; Ghosh S. ; Alejandro Martinez J. ; Dominguez F. ; Kumar P.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2017
卷: 30, 期: 5 起始页码: 1839
结束页码: 1859
语种: 英语
Scopus关键词: Atmospheric thermodynamics
; Oceanography
; Rain
; Upper atmosphere
; Atmospheric moisture
; Indian summer monsoon rainfall
; Interannual variability
; Lagrangian trajectories
; Ocean-atmosphere interactions
; Relative contribution
; Seasonal and interannual variability
; Western indian oceans
; Moisture
; air-sea interaction
; annual variation
; El Nino
; moisture transfer
; monsoon
; rainfall
; seasonal variation
; summer
; Ganges Basin
; Indian Ocean
英文摘要: Three key issues of moisture supply and Indian summer monsoon rainfall (ISMR) variability are discussed in the present work: identification of the oceanic and terrestrial sources of moisture; the extent to which each source affects the ISMR; and their individual contributions to the interannual variability of ISMR. The modified Dynamic Recycling Model, based on a Lagrangian trajectory approach, is used to estimate the relative contributions from 27 terrestrial and oceanic moisture source regions to the monsoon during 1979-2013. ERA-Interim data are used for the study. The results show that the ISMR is strongly influenced by the land-ocean-atmosphere interactions, a significant fraction of atmospheric moisture to the ISMR comes from five main moisture sources: the western Indian Ocean (WIO), central Indian Ocean (CIO), upper Indian Ocean (UIO), Ganges basin (GB), Red Sea and the neighboring gulf (RDG). The moisture flux from WIO is very high during the initial period of monsoon seasons. From the mid-monsoon season, the contribution from this moisture source decays and land sources through evapotranspiration (ET) become more active. Early decay of moisture contributions from the WIO and the GB is observed during weak monsoon years. El Niño years are associated with low contributions of moisture from all sources, whereas warm Indian Ocean years are associated with low moisture flux from the major sources except WIO. ISMR is characterized by the prolonged and increasing moisture supply from WIO during the first half of the monsoon along with contributions from GB during the end of season. The results are consistent across several reanalyses (CFSR, ERA-Interim, MERRA). © 2017 American Meteorological Society. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/49789
Appears in Collections: 气候变化事实与影响
There are no files associated with this item.
作者单位: Department of Civil Engineering, Indian Institute of Technology Bombay, Mumbai, India; Department of Civil Engineering, Interdisciplinary Program in Climate Studies, Indian Institute of Technology Bombay, Mumbai, India; Institute of Physics, University of Antioquia, Medellin, Colombia; Department of Atmospheric Sciences, University of Illinois at Urbana-Champaign, Urbana, IL, United States; Civil and Environmental Engineering, University of Illinois at Urbana-Champaign, Urbana, IL, United States
Recommended Citation:
Pathak A.,Ghosh S.,Alejandro Martinez J.,et al. Role of oceanic and land moisture sources and transport in the seasonal and interannual variability of summer monsoon in India[J]. Journal of Climate,2017-01-01,30(5)