Quantifying rates of climate change in mountain regions is of considerable interest, not least
because mountains are viewed as climate “hotspots” where change can anticipate or …

Warming amplification over the Arctic Pole (AP hereafter) and Third Pole (Tibetan Plateau,
TP hereafter) can trigger a series of climate responses and have global consequences …

Abstract The latest Coupled Model Intercomparison Project phase 6 (CMIP6) dataset was
analyzed to examine the projected changes in temperature and precipitation over six South …

Abstract The Tibetan Plateau (TP) is also known as the “Third Pole”. Elevation dependent
warming (EDW), the phenomenon that warming rate changes systematically with elevation …

• Future climate projections under various CMIP5 scenarios suggest warming of the HKH
region in the range of 2.6–4.6 C by the end of the twenty-first century. While future …

The hydrological response to climate change in mountainous basins manifests itself at
varying spatial and temporal scales, ranging from catchment to large river basin scale and …

Climate change is a phenomenon that is unequivocally altering the natural systems in all
parts of the world but the alteration in climate extremes may pose more severe and …

Research on the Himalayan cryosphere has increasingly focused on climate change,
considering aspects such as snow cover dynamics, precipitation and temperature trends …

Regional climate change (CC) and land use changes (LUCs) can significantly influence the
hydrological processes at watershed scale. Different studies have investigated the impact of …

This study focused on the trends of rainfall variability and drought monitoring in the northern
region of Pakistan (Gilgit-Baltistan). Climate Hazards Group Infrared Precipitation with …