Abstract:
The hydrology of the Himalayan region and its changes are being closely
watched today as it is vital for the sustenance of a very large mountain
population as well as the people in the plains downstream. Several of the big
rivers originate in the Himalaya and civilizations are built and sustained in its
flood plains. Today, with the increasing population and unpredictable climate,
water resources in the region is experiencing an unprecedented stress.
Regionally, mountain communities are trying to cope with greater uncertainty
of water related issues, such as floods and water availability. These scenarios
forces us to look into the finer details of the water resources dynamics in the
Himalayas. The Himalaya is known for its glaciers and snow cover from time
immemorial and during the past decades, most of the attention focused on these
two cryospheric components. The climate change debates during the past two
decades have given a fillip for the Himalayan glacier research and an increased
vigour in research activities are visible today on this front. However, knowledge
about frozen ground, and more specifically permafrost in the high altitude
regions of the Himalaya is sparse till date. Permafrost is the thermal state of
ground material, which remains at or below 0oC for more than two years.
However, normally frozen water is part of permafrost. The layer above
permafrost is termed ‘active layer’ and thaws during the warm season. A lack
of appreciation of permafrost stems primarily from the fact that it is hidden
beneath the ground surface. Furthermore, the impact of thawing permafrost on
the mountain eco-system in comparison to other cryospheric components is
largely unknown. However, recent studies have suggested widespread
occurrence of permafrost in the Himalayan region and its potential role in
local/regional water availability as well as disasters such as landslides. This is
especially true for the arid regions of the Himalaya and more so under the
changing climate. As permafrost lies beneath the ground, we need to employ
robust monitoring and modeling strategies to understand the permafrost and its
characteristics in the Himalayan region. To achieve this, we need trained and
dedicated manpower as well as sufficient funds to undertake research in the high
altitude terrain, and institutions with committed programmes to sustain such
research activities and capacity building. Hence the workshop was aiming at
bringing together various national and international stakeholders with following
objectives a) Sensitize the local government, funding agencies, research
institutions, universities and other stakeholders on various issues related to the
permafrost thaw/ ground ice in the Himalaya with an aim to promote permafrost
research and knowledge generation in the Indian Himalayan region (IHR) and
b) Explore research collaborations with experts in the field who can help in
fostering permafrost research in India.Wide appreciation of the knowledge gap and need for permafrost and
frozen ground research in the Himalayan region.
Identification of key problem areas: A. Lack of research background in
Indian institutions and universities B. Lack of funding opportunities for
permafrost/frozen ground research.
Establishment of Indian Permafrost Network (IPN) with National Institute
of Hydrology, Roorkee as the lead organisation.
Expression of interest to be part of the Permafrost Network by 25
Individual members belonging to 15 institutions.
Identification of thrust areas for permafrost research in the Himalayan
region 1. Field monitoring (Ground temperature) 2. Hydrology 3.
Modelling 4. Chemistry and isotope studies 5. Kinematics and Dynamics
6. Remote Sensing 7. Geophysical Survey 8. Instrumentation and Sensors.
Identified organisation of a training programme and project mentoring as
immediate next step to promote permafrost research in the country.
Willingness of international participants/institutions in collaborations for
training and research