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High-resolution climate change projection of northeast monsoon rainfall over peninsular India
Corresponding Author
C. B. Jayasankar
Center for Study of Science, Technology & Policy (CSTEP), Bangalore, India
Correspondence
C. B. Jayasankar, Center for Study of Science, Technology & Policy (CSTEP), Bangalore, India.
Email: [email protected]
Search for more papers by this authorK. Rajendran
CSIR Fourth Paradigm Institute (CSIR-4PI), NAL Belur Campus, Bangalore, India
Academy of Scientific and Innovative Research (AcSIR), CSIR-4PI, Bangalore, India
Search for more papers by this authorSurendran Sajani
CSIR Fourth Paradigm Institute (CSIR-4PI), NAL Belur Campus, Bangalore, India
Academy of Scientific and Innovative Research (AcSIR), CSIR-4PI, Bangalore, India
Search for more papers by this authorK. V. Ajay Anand
CSIR Fourth Paradigm Institute (CSIR-4PI), NAL Belur Campus, Bangalore, India
Search for more papers by this authorCorresponding Author
C. B. Jayasankar
Center for Study of Science, Technology & Policy (CSTEP), Bangalore, India
Correspondence
C. B. Jayasankar, Center for Study of Science, Technology & Policy (CSTEP), Bangalore, India.
Email: [email protected]
Search for more papers by this authorK. Rajendran
CSIR Fourth Paradigm Institute (CSIR-4PI), NAL Belur Campus, Bangalore, India
Academy of Scientific and Innovative Research (AcSIR), CSIR-4PI, Bangalore, India
Search for more papers by this authorSurendran Sajani
CSIR Fourth Paradigm Institute (CSIR-4PI), NAL Belur Campus, Bangalore, India
Academy of Scientific and Innovative Research (AcSIR), CSIR-4PI, Bangalore, India
Search for more papers by this authorK. V. Ajay Anand
CSIR Fourth Paradigm Institute (CSIR-4PI), NAL Belur Campus, Bangalore, India
Search for more papers by this authorFunding information: None
Abstract
In this study, projected changes in mean northeast monsoon (NEM) rainfall and associated extreme rainfall and temperature events, over peninsular India (PI) and its six subdivisions, are quantified. High-resolution dynamically downscaled simulations of the Weather Research and Forecasting (WRF) regional climate model driven by the boundary conditions from the Community Climate System Model version 4 (CCSM4) model (WRF-CCSM4) are compared with statistically downscaled simulations of NASA Earth Exchange Global Daily Downscaled Projections (NEX-GDDP). Over PI, these downscaled simulations show low bias in mean NEM rainfall (≤ − 0.44 mm·day−1) and high pattern correlation coefficient (≥0.75), giving confidence in their future projections. Under future warming over PI, both downscaled simulations project future significant enhancement in NEM rainfall with WRF-CCSM4 projecting 1.98 mm·day−1 (83.78% change with respect to the present-day mean) whereas the multimodel ensemble (MME) of eight NEX-GDDP models project 0.67 ± 0.58 mm·day−1 (19.78%) by the midddle of the century and 1.42 ± 0.97 mm·day−1 (42.76%) by the end of the century. Analysis of extreme rainfall events shows that WRF-CCSM4 projects future enhancement (reduction) in extreme rainfall (R95p) days over 91.4% (8.6%) of grid-points over PI. In future, coastal areas of Karnataka and Andhra Pradesh will likely experience increased extreme rainfall occurrence by more than 25 days and 15–20 days respectively. Projected future enhancement in the mean and extreme NEM rainfall is attributed to the increased precipitable water under a warming climate. Future projection of extreme temperature indices shows an increase in minimum and maximum temperatures over PI during the NEM season. Over PI, future winter nights and days are found to be warmer than those in the present day and the temperature change in future winter nights is found to be larger than that in winter days. This climate change information would help decision-makers in evaluating existing policies and devising revised policies to reduce risk due to climate change.
CONFLICT OF INTEREST
There is no conflict of interest.
Supporting Information
Filename | Description |
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qj4017-sup-0001-AppendixS1.docxapplication/unknown, 929.4 KB | TABLE S1 Details such as the parent model name, horizontal resolution of the atmospheric model and the name of the modelling center for eight NASA Earth Exchange Global Daily Downscaled Projections (NEX-GDDP) simulations used in the present study. |
qj4017-sup-0001-AppendixS1.docxapplication/unknown, 929.4 KB | TABLE S2 Observed long-term (1971–2000) annual mean and northeast monsoon (NEM) rainfall (in mm) from high-resolution IMD rainfall data. Also shown are the percentage of NEM rainfall with respect to the annual mean for all India (AI), peninsular India (PI) and its six subdivisions. |
qj4017-sup-0001-AppendixS1.docxapplication/unknown, 929.4 KB | TABLE S3 Projected change in northeast monsoon rainfall (mm·day−1) and the percentage change with respect to present-day rainfall over peninsular India (PI) and its six meteorological subdivisions from NEX-CCSM4 model for the mid of the century and end of the century. Area averaging is performed only over grids with changes significant at 95% level and values with + symbol are through area averaging over grids with changes significant at 80% level. |
qj4017-sup-0001-AppendixS1.docxapplication/unknown, 929.4 KB | FIGURE S1 Climatological mean northeast monsoon rainfall bias for eight NEX-GDDP models along with their MME with respect to the IMD observation for the period 1971–2000. |
qj4017-sup-0001-AppendixS1.docxapplication/unknown, 929.4 KB | FIGURE S2 Climatological mean northeast monsoon rainfall bias for WRF-CCSM4 with respect to the IMD observation for the period 1981–1990. |
qj4017-sup-0001-AppendixS1.docxapplication/unknown, 929.4 KB | FIGURE S3 Projected change in climatological mean northeast monsoon rainfall over peninsular India from WRF-CCSM4 during the end of the 21st century. Grids points significant at 95% is marked with dots. |
qj4017-sup-0001-AppendixS1.docxapplication/unknown, 929.4 KB | FIGURE S4 Projected change in climatological mean northeast monsoon rainfall over peninsular India from eight NEX-GDDP models and their MME during the mid of the 21st century. |
qj4017-sup-0001-AppendixS1.docxapplication/unknown, 929.4 KB | FIGURE S5 Projected change in climatological mean northeast monsoon rainfall over peninsular India from eight NEX-GDDP models and their MME during the end of the 21st century. |
Please note: The publisher is not responsible for the content or functionality of any supporting information supplied by the authors. Any queries (other than missing content) should be directed to the corresponding author for the article.
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