From atop the 13,600-ft high windswept crest of a steep, serrated ridge, the Samudra Tapu glacier is a giant blanket of ice and snow, covering the bowl-shaped valley between jagged Himalayan peaks
Climatic changes, droughts, floods, heat/cold waves, pests, diseases and poverty dynamics is a complex phenomenon demanding multidisciplinary management of early warning systems, risk assessment, insurance and mitigation.
The Arctic climate is changing. Permafrost is warming, hydrological processes are changing and biological and social systems are also evolving in response to these changing conditions. Knowing how the structure and function of arctic terrestrial ecosystems are responding to recent and persistent climate change is paramount to understanding the future state of the Earth system and how
Melting Himalayan glaciers are threatening to unleash a torrent of floods into mountain valleys, and ultimately dry up rivers across South Asia. A new study, due to be presented in July to the International Commission on Snow and Ice (ICSI), predicts that most of the glaciers in the region will vanish within 40 years as a result of global warming.
To study the role of snow and ice in the global watercycle and in the world climatic system, research methods should be further standardized and inform from different region integrated. Representing these field of research, the International Commission on Snow and Ice (ICSI) has already made some guideline studies on the runoff prediction and evaluation.
Glaciers that feed the Indus River in Pakistan’s Karakoram mountains are melting faster than previously thought. Saleem Sheikh talks to the scientists behind the latest field research that contradicts earlier satellite studies showing glaciers are relatively stable.