Projected and Observed Aridity and Climate Change in the East Coast of South India under RCP 4.5
In the purview of global warming, the present study attempts to project changes in climate and quantify the changes in aridity of two coastal districts in south India under the RCP 4.5 trajectory. Projected climate change output generated by RegCM 4.4 model, pertaining to 14 grid points located with...
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doaj-92e7923d6a344f609097aff1e4deb4f62020-11-25T02:00:33ZengHindawi LimitedThe Scientific World Journal2356-61401537-744X2015-01-01201510.1155/2015/169761169761Projected and Observed Aridity and Climate Change in the East Coast of South India under RCP 4.5A. Ramachandran0Dhanya Praveen1R. Jaganathan2K. Palanivelu3Centre for Climate Change and Adaptation Research, Anna University, Guindy, Chennai 600025, IndiaCentre for Climate Change and Adaptation Research, Anna University, Guindy, Chennai 600025, IndiaTamil Nadu Agricultural University, Coimbatore, Tamil Nadu 641003, IndiaCentre for Climate Change and Adaptation Research, Anna University, Guindy, Chennai 600025, IndiaIn the purview of global warming, the present study attempts to project changes in climate and quantify the changes in aridity of two coastal districts in south India under the RCP 4.5 trajectory. Projected climate change output generated by RegCM 4.4 model, pertaining to 14 grid points located within the study area, was analyzed and processed for this purpose. The meteorological parameters temperature and precipitations were used to create De Martonne Aridity Index, to assess the spatial distribution of aridity. The original index values ranged from 13.7 to 16.4 mm/°C, characterizing this area as a semidry climate. The outcome from the changed scenario analysis under RCP 4.5 showed that, during the end of the 21st century, the aridity may be increased more as the index values tend to reduce. The increasing trend in the drying phenomenon may be attributed to the rising of mean annual temperatures.http://dx.doi.org/10.1155/2015/169761 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
A. Ramachandran Dhanya Praveen R. Jaganathan K. Palanivelu |
spellingShingle |
A. Ramachandran Dhanya Praveen R. Jaganathan K. Palanivelu Projected and Observed Aridity and Climate Change in the East Coast of South India under RCP 4.5 The Scientific World Journal |
author_facet |
A. Ramachandran Dhanya Praveen R. Jaganathan K. Palanivelu |
author_sort |
A. Ramachandran |
title |
Projected and Observed Aridity and Climate Change in the East Coast of South India under RCP 4.5 |
title_short |
Projected and Observed Aridity and Climate Change in the East Coast of South India under RCP 4.5 |
title_full |
Projected and Observed Aridity and Climate Change in the East Coast of South India under RCP 4.5 |
title_fullStr |
Projected and Observed Aridity and Climate Change in the East Coast of South India under RCP 4.5 |
title_full_unstemmed |
Projected and Observed Aridity and Climate Change in the East Coast of South India under RCP 4.5 |
title_sort |
projected and observed aridity and climate change in the east coast of south india under rcp 4.5 |
publisher |
Hindawi Limited |
series |
The Scientific World Journal |
issn |
2356-6140 1537-744X |
publishDate |
2015-01-01 |
description |
In the purview of global warming, the present study attempts to project changes in climate and quantify the changes in aridity of two coastal districts in south India under the RCP 4.5 trajectory. Projected climate change output generated by RegCM 4.4 model, pertaining to 14 grid points located within the study area, was analyzed and processed for this purpose. The meteorological parameters temperature and precipitations were used to create De Martonne Aridity Index, to assess the spatial distribution of aridity. The original index values ranged from 13.7 to 16.4 mm/°C, characterizing this area as a semidry climate. The outcome from the changed scenario analysis under RCP 4.5 showed that, during the end of the 21st century, the aridity may be increased more as the index values tend to reduce. The increasing trend in the drying phenomenon may be attributed to the rising of mean annual temperatures. |
url |
http://dx.doi.org/10.1155/2015/169761 |
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