This paper presents a review of Late Quaternary climatic changes and glacier variability in
the Himalaya and East Africa, focusing on the role of Indian Summer Monsoon (ISM), East …

As one of the most prominent seasonally recurring atmospheric circulation patterns, the
Asian summer monsoon (ASM) plays a vital role for the life and livelihood of about one-third …

Stable isotope records from speleothems provide information on past climate changes, most
particularly information that can be used to reconstruct past changes in precipitation and …

Comprehensive comparison of paleoclimate change based on records constrained by
precise chronology and high-resolution is essential to explore the correlation and interaction …

Abstract The Bay of Bengal (BoB) is a semi-enclosed basin located in the north-eastern
Indian Ocean which receives enormous fluvial sediment input primarily from the Himalayan …

Gangotri glacier, located in the Uttarkashi district, is one of the longest valley glaciers of the
Garhwal Himalaya. It exhibits lateral moraines, recessional moraines, outwash plains, kame …

Speleothems, particularly stalagmites are extensively used to reconstruct paleoclimatic and
paleomonsoon changes by using stable oxygen and carbon isotopes along the growth …

We present a stalagmite based high resolution climatic record between∼ 4.0 and 1.9 ka BP
from Dharamjali Cave in Pithoragarh (Kumaun Himalaya), an area which is influenced …

We present results of our investigations on 7.65 m long core sediments from the Khajjiar
lake, Himachal Pradesh, aimed at reconstructing palaeoclimate variability in the climatically …

Speleothem oxygen isotope (δ 18 O) constitutes one of key proxies to reconstruct the Indian
and East Asian summer monsoon (ISM and EASM) hydroclimate history on a wide range of …