The Indian summer monsoon rainfall (ISMR) during June to September contributes most of
the annual rainfall over India and plays an important role in Indian agriculture and thus the …

The transitions of short-term trends of Indian Summer Monsoon daily precipitation extremes
remain poorly understood. Here, we show a short-term declination of temporal frequency of …

The dipole pattern (wetting over northwestern India and drying over the Indo-Gangetic plains
and northeast India) in the rainfall trends is reported in many earlier studies. The exact …

Cyclonic low‐pressure systems (LPS) produce abundant rainfall in South Asia, where they
are traditionally categorized as monsoon lows, monsoon depressions, and more intense …

This study makes the case that monsoon depressions over South Asia can form from a
variant of moist barotropic instability. Using an idealized numerical framework in which the …

During the pre-monsoon season, the Northwest Himalayas region receives a significantly
larger proportion of precipitation than the pan Indian average. This heightened precipitation …

The Indian summer monsoon rainfall (ISMR) exhibits significant variability, affecting the food
and water security of the densely populated Indian subcontinent. The two dominant spatial …

Somali upwelling system during northern summer is believed to be the largest upwelling
region in the Indian Ocean and has motivated some of the early studies on the Indian …

Relative humidity (RH), an important climatic element influencing tree growth, is also crucial
in assessing the General Circulation Models (GCMs) on global warming. However, in the …

Historical trends in monsoon low pressure systems (LPS), the dominant rain-bearing
weather system of South Asia, have been difficult to assess due to changes in the observing …