Displaying results 1 - 20 of 1777 matches (0.02 seconds)
The Indus River Basin is shared by four countries Afghanistan, China, India, and Pakistan, with the largest portions of the basin lying in Pakistan (52%) and India (33%). The main river originates at Lake Ngangla Rinco on the Tibetan Plateau in the
entitled, Gender Analysis of Climate Change Impacts and Adaptation in China with Focus on Yunnan. More than 30 representatives from
Rural Livelihoods and Climate Change Adaptation in the Himalayas (Himalica) Initiative is financed by the European Union and aims to support poor and vulnerable mountain communities in the Hindu Kush Himalayan (HKH) region in mitigating and
of Environment, Forestry & Climate Change (MoEF&CC) kicked off the soft launch of Climate+Change Indian Himalayan Region: Our Mountains Our Future during a ceremony on 15 December 2016 at the MoEF&CC’s new Indira
particularly vulnerable to climate change. The high peaks of the Himalayas are a vast storehouse of water in frozen form, with the world’s greatest concentration of
The certification programme seeks to build knowledge and capacity in local leaders, with a particular focus to assist poor and marginalized communities in preparing for future disasters.
The Hindu Kush Himalaya (HKH), a global asset, is rich in cultural and biological diversity, and natural resources. It is also home to inaccessible, remote, and fragile regions where local populations live in poverty. Managing ecosystems in the
Change continued its roll across the Himalayas in 2015 with its arrival in New Delhi, launching the Indian segment of the open-ended initiative that combines an evolving exhibition with outreach, documentation, creative expression, and
SWFG operates in Kalchebesi, a small village of about 25 households situated in Patlekhet, a village development committee in Kavre District. The village is located 46 kilometres east of Kathmandu, the capital city of Nepal. Most of the people here
Conference on Biodiversity, Climate Change Assessment, and Impacts on Livelihood was organized in Kathmandu from 10-12 January 2017. The three-day event brought together 300 national and 100 international scientists, policy makers, and
“Himalayan Adaptation, Water and Resilience (HI-AWARE) Research on Glacier and Snowpack Dependent River Basins for Improving Livelihoods” is a five year study that ICIMOD is leading with its partners in four river basins namely Indus, Upper
journalists on reporting climate change adaptation was organised by the International Centre for Integrated Mountain Development (ICIMOD) in Nyaung Shwe, Shan State, in collaboration with the Myanmar Institute for
on the Cryosphere in a Changing Climate was held in Wellington, New Zealand, from 12 to 17 February 2017. The symposium brought together renowned glaciologists from around the world to discuss and share research findings on
HI-AWARE – a research programme on adaptation, water, and resilience in glacier and snowpack dependent river basins of the region – brought together policy makers and practitioners from Nepal for a two-day workshop to share initial results of
How is climate change impacting water resources in the Himalayas? That’s a big question, and now there’s a comprehensive atlas that policy makers and practitioners can turn to for answers and information.
Many records indicate that the trend of rising temperatures is more significant in mountain regions than adjacent lowlands. Climate models also suggest that the future will bring greater temperature increase and more erratic precipitation.
web app on climate change vulnerability of forest ecosystems provides information about the current relationships between climate variables and biophysical variables depicting functioning of forests. The application also provides VDC level
knowledge generating and exchange institutions both within and
title, “Gender Analysis of Climate Change Impacts and Adaptation in China with Focus on Yunnan” was held in Baoshan City, Yunnan, China, on 15 March 2017. Many of the case studies presented in this book are
potentially affected by changes in permafrost. Permafrost is ground material (rock or soil) at or below 0 degrees C for two or more years. The surface layer