TY - JOUR
T1 - Climate change detection and attribution in the Ganga-Brahmaputra-Meghna river basins
AU - Sharma, Chetan
AU - Shukla, Anoop Kumar
AU - Zhang, Yongqiang
N1 - Funding Information:
This research was jointly supported by the Second Tibetan Plateau Scientific Expedition and Research Program (2019QZKK0208) and CAS Pioneer Hundred Talents Program. The authors thank the CRU, NERC UK and NCEP/NCAR, NOAA/OAR/ESRL PSL, Boulder, Colorado, USA, for providing the monthly observed precipitation and reanalysis data. The authors are also thankful to the anonymous reviewers for their constructive suggestions to improve the quality of the present work. Monthly observed precipitation data used in this study can be obtained from https://crudata.uea.ac.uk/cru/data/hrg/. Reanalysis data was obtained from NCEP/NCAR (available at https://www.esrl.noaa.gov/psd/data/gridded/data.ncep.reanalysis.html). CMIP5 GCM variable can be downloaded from https://esgf-node.llnl.gov/projects/cmip5/. Some or all data, models, or codes generated during the study are available from the corresponding author by request.
Funding Information:
This research was jointly supported by the Second Tibetan Plateau Scientific Expedition and Research Program (2019QZKK0208) and CAS Pioneer Hundred Talents Program. The authors thank the CRU, NERC UK and NCEP/NCAR, NOAA/OAR/ESRL PSL, Boulder, Colorado, USA, for providing the monthly observed precipitation and reanalysis data. The authors are also thankful to the anonymous reviewers for their constructive suggestions to improve the quality of the present work.
Publisher Copyright:
© 2021 China University of Geosciences (Beijing) and Peking University
PY - 2021/9
Y1 - 2021/9
N2 - Ganga-Brahmaputra-Meghna (GBM) river basin is the third-largest and one of the most populated river basins in the world. As climate change is affecting most of the hydrometeorological variables across the globe, this study investigated the existence of climate change signal in all four climatological seasons in the GBM river basin and assessed the contribution of anthropogenic activities, i.e., Greenhouse Gases (GHGs) emission in the change. Significant decreasing trends in the monsoon and a small increase in pre-monsoon precipitation were observed. Negligible change was detected in post-monsoon and winter season precipitation. CMIP5 GCMs were used for climate change detection, change point estimation, and attribution studies. Support Vector Machine (SVM) regression method was adopted to downscale GCM variables at the local scale. Monte-Carlo simulation approach was used to detect changes in different seasons. The climate change ‘signals’ were detectable after the year 1980 using Signal to Noise ratio (SNR) method in the majority of central and north-western regions. The change point was detectable only in annual monsoon precipitation at the basin level. Attribution analysis indicated >50% contribution of anthropogenic activities (GHGs) to annual monsoon precipitation changes. So, there is high confidence that monsoon precipitation in GBM has significantly changed due to anthropogenic activities. Different mitigation and adaption measures are also suggested, which may be adopted to manage the growing demand and water availability in the basin.
AB - Ganga-Brahmaputra-Meghna (GBM) river basin is the third-largest and one of the most populated river basins in the world. As climate change is affecting most of the hydrometeorological variables across the globe, this study investigated the existence of climate change signal in all four climatological seasons in the GBM river basin and assessed the contribution of anthropogenic activities, i.e., Greenhouse Gases (GHGs) emission in the change. Significant decreasing trends in the monsoon and a small increase in pre-monsoon precipitation were observed. Negligible change was detected in post-monsoon and winter season precipitation. CMIP5 GCMs were used for climate change detection, change point estimation, and attribution studies. Support Vector Machine (SVM) regression method was adopted to downscale GCM variables at the local scale. Monte-Carlo simulation approach was used to detect changes in different seasons. The climate change ‘signals’ were detectable after the year 1980 using Signal to Noise ratio (SNR) method in the majority of central and north-western regions. The change point was detectable only in annual monsoon precipitation at the basin level. Attribution analysis indicated >50% contribution of anthropogenic activities (GHGs) to annual monsoon precipitation changes. So, there is high confidence that monsoon precipitation in GBM has significantly changed due to anthropogenic activities. Different mitigation and adaption measures are also suggested, which may be adopted to manage the growing demand and water availability in the basin.
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U2 - 10.1016/j.gsf.2021.101186
DO - 10.1016/j.gsf.2021.101186
M3 - Article
AN - SCOPUS:85104122607
SN - 1674-9871
VL - 12
JO - Geoscience Frontiers
JF - Geoscience Frontiers
IS - 5
M1 - 101186
ER -