| dc.contributor.author |
HARI V. |
|
| dc.contributor.author |
GHOSH S. |
|
| dc.contributor.author |
ZHANG W. |
|
| dc.contributor.author |
KUMAR R. |
|
| dc.date.accessioned |
2023-03-17T04:35:41Z |
|
| dc.date.available |
2023-03-17T04:35:41Z |
|
| dc.date.issued |
2022 |
|
| dc.identifier.citation |
Nature Communications,13(1) |
en_US |
| dc.identifier.issn |
20411723 |
|
| dc.identifier.uri |
https://dx.doi.org/10.1038/s41467-022-32942-5 |
|
| dc.identifier.uri |
http://localhost:8080/xmlui/handle/100/37304 |
|
| dc.description.abstract |
Increased occurrence of heatwaves across different parts of the world is one of the characteristic signatures of anthropogenic warming. With a 1.3 billion population, india is one of the hot spots that experience deadly heatwaves during may-june – yet the large-scale physical mechanism and teleconnection patterns driving such events remain poorly understood. Here using observations and controlled climate model experiments, we demonstrate a significant footprint of the far-reaching pacific meridional mode (pmm) on the heatwave intensity (and duration) across north central india (nci) – the high risk region prone to heatwaves. A strong positive phase of pmm leads to a significant increase in heatwave intensity and duration over nci (0.8-2 °c and 3–6 days; p < 0.05) and vice-versa. The current generation (cmip6) climate models that adequately capture the pmm and their responses to nci heatwaves, project significantly higher intensities of future heatwaves (0.5-1 °c; p < 0.05) compared to all model ensembles. These differences in the intensities of heatwaves could significantly increase the mortality (by ≈150%) and therefore can have substantial implications on designing the mitigation and adaptation strategies. © 2022, the author(s). |
en_US |
| dc.language.iso |
English |
en_US |
| dc.publisher |
Nature Research |
en_US |
| dc.subject.other |
adaptation |
en_US |
| dc.subject.other |
climate modeling |
en_US |
| dc.subject.other |
heat wave |
en_US |
| dc.subject.other |
mitigation |
en_US |
| dc.subject.other |
mortality |
en_US |
| dc.subject.other |
article |
en_US |
| dc.subject.other |
climate model |
en_US |
| dc.subject.other |
heat wave |
en_US |
| dc.subject.other |
India |
en_US |
| dc.subject.other |
mitigation |
en_US |
| dc.subject.other |
mortality |
en_US |
| dc.subject.other |
Pacific Ocean |
en_US |
| dc.subject.other |
summer |
en_US |
| dc.subject.other |
acclimatization |
en_US |
| dc.subject.other |
infrared radiation |
en_US |
| dc.subject.other |
Pacific Ocean |
en_US |
| dc.subject.other |
season |
en_US |
| dc.subject.other |
India |
en_US |
| dc.subject.other |
Pacific Ocean |
en_US |
| dc.subject.other |
Acclimatization |
en_US |
| dc.subject.other |
India |
en_US |
| dc.subject.other |
Infrared Rays |
en_US |
| dc.subject.other |
Pacific Ocean |
en_US |
| dc.subject.other |
Seasons |
en_US |
| dc.title |
Strong influence of north Pacific Ocean variability on Indian summer heatwaves |
en_US |
| dc.type |
Article |
en_US |