Ozone and UV bulletin
The stratosphere ozone layer is slowly recovering and the recovery will be complete in most parts of the atmosphere in the coming decades, according to the latest bulletin by the World Meteorological Organization
The stratosphere ozone layer is slowly recovering and the recovery will be complete in most parts of the atmosphere in the coming decades, according to the latest bulletin by the World Meteorological Organization
Cold winds blowing from the western Himalayan region brought down Delhi’s maximum temperature by seven degrees between Thursday and Friday. The day temperature on Friday settled at 21.6 degrees Celsius,
This year, the arrival of southwest monsoon current over the south Bay of Bengal and south Andaman Sea was delayed by 3 days due to non-conducive conditions for the development of convection over the region
Flash floods on the edge of high terrain, such as the Himalayas or Rocky Mountains, are especially dangerous and hard to predict. The Leh flood of 2010 at the edge of the Himalayan Plateau in India is
A report to the 24th Meeting of Parties to the Montreal Protocol on Substances that Deplete the Ozone Layer, celebrating past achievements and looking ahead to future challenges.
BHUBANESWAR: The South West Monsoon withdrew from most parts of Odisha on Monday signalling the end of rainy season which recorded a rare zero percent deviation this year. The India Meteorological Department
The main objective of this note is to affirm that if trend of all-India rainfall, 4 weeks in advance is the sought objective, then this is achievable; in particular, this applies to the Indian summer monsoon
Data are presented that support the idea of an oxygenation event in the immediate aftermath of the Marinoan glaciation, pre-dating previous estimates for post-Marinoan oxygenation by more than 50 million
Tropical cyclones over the Arabian Sea in the pre-monsoon season (May–June) have intensified since 1997 owing to significant reductions in storm-ambient vertical wind shear (VWS) in the troposphere; these
Arabian Sea tropical cyclones have become stronger over the past 30 years owing to a reduction in vertical wind shear (VWS) brought about by radiative forcing from pollution aerosols1. Wang et al.2 argue
Analysis of observations on six continents reveals a global preference for afternoon rain to fall on locally drier soils—contrary to the predictions of large-scale climate models, and suggesting that such