globalchange  > 气候减缓与适应
DOI: 10.1002/joc.5216
论文题名:
Investigation of temperature changes over India in association with meteorological parameters in a warming climate
作者: Purnadurga G.; Lakshmi Kumar T.V.; Koteswara Rao K.; Rajasekhar M.; Narayanan M.S.
刊名: International Journal of Climatology
ISSN: 8998418
出版年: 2018
卷: 38, 期:2
起始页码: 867
结束页码: 877
语种: 英语
英文关键词: India ; mass stream function ; maximum temperatures ; OLR ; pet
Scopus关键词: Climate change ; Polyethylene terephthalates ; Spectrum analysis ; India ; Linear associations ; Maximum temperature ; Meridional velocities ; Meteorological parameters ; Outgoing longwave radiation ; Potential evapotranspiration ; Streamfunctions ; Atmospheric temperature ; air temperature ; atmospheric moisture ; data set ; meteorology ; regression analysis ; summer ; warming ; India
英文摘要: We have used 1° × 1° resolution maximum temperature (TMAX) data sets developed by India Meteorological Department (IMD) to examine the summer time warming over India during the period 2001–2014 in comparison with the period 1971–2000. The two study periods have been arrived at based on the drastic change of Moisture Index (IM) trends over India between the two epochs. The TMAX variations over India are discussed with the corresponding changes in Potential Evapotranspiration (PET) data of the Climate Research Unit (CRU) and Outgoing Longwave Radiation (OLR) data of NOAA ESRL. The study shows a considerable warming over northern parts of India compared to southern parts. Western Himalayas (WH) and Northwest (NW) regions experienced highest warming with 1.4 °C and 0.8 °C increases during Epoch 2 (2001–2014) as compared Epoch 1 (1971–2000) during the summer (March, April and May). Using MERRA Black Carbon Surface Mass Concentration (BCSMC) data, we have analysed the relation of increasing BCSMC with the TMAX over different homogeneous temperature regions of India and found that BCSMC has increased upto 1.6 times between the two epochs. Strong linear association is found between TMAX, PET and OLR evidenced by Coherence Wavelet Spectral analysis. It is also found that the highest warming occurred in the month of March and is 2.2 °C in WH and 1.4 °C in NW parts of India. We calculated mass stream function based on zonal mean meridional velocity for the two periods. In the recent periods we observed the weakening of polar cell and northward expansion of Hadley cell. These changes may be related to warming conditions of the atmosphere which may explain the intensification and northward expansion of the Ferrel cell with favourable conditions during the summer season. © 2017 Royal Meteorological Society
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/117086
Appears in Collections:气候减缓与适应

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作者单位: Department of Physics, Atmospheric Science Research Laboratory, SRM University, Chennai, India; School of Earth and Environmental sciences, Seoul National University, Seoul, South Korea; Sathish Dhawan Space Centre, ISRO, Srihari Kota, India; DRVE, SRM University, Chennai, India

Recommended Citation:
Purnadurga G.,Lakshmi Kumar T.V.,Koteswara Rao K.,et al. Investigation of temperature changes over India in association with meteorological parameters in a warming climate[J]. International Journal of Climatology,2018-01-01,38(2)
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