Warming amplification over the Arctic Pole and Third Pole: Trends, mechanisms and consequences
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 …
TP hereafter) can trigger a series of climate responses and have global consequences …
Elevation dependent warming over the Tibetan Plateau: Patterns, mechanisms and perspectives
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 …
warming (EDW), the phenomenon that warming rate changes systematically with elevation …
High mountain areas
The cryosphere (including, snow, glaciers, permafrost, lake and river ice) is an integral
element of high mountain regions, which are home to roughly 10% of the global population …
element of high mountain regions, which are home to roughly 10% of the global population …
Global variation in diurnal asymmetry in temperature, cloud cover, specific humidity and precipitation and its association with leaf area index
The impacts of the changing climate on the biological world vary across latitudes, habitats
and spatial scales. By contrast, the time of day at which these changes are occurring has …
and spatial scales. By contrast, the time of day at which these changes are occurring has …
Does the climate warming hiatus exist over the Tibetan Plateau?
A Duan, Z **ao - Scientific reports, 2015 - nature.com
The surface air temperature change over the Tibetan Plateau is determined based on
historical observations from 1980 to 2013. In contrast to the cooling trend in the rest of China …
historical observations from 1980 to 2013. In contrast to the cooling trend in the rest of China …
[HTML][HTML] Climate change impact assessment on the hydrological regime of the Kaligandaki Basin, Nepal
Abstract The Hindu Kush-Himalayan region is an important global freshwater resource. The
hydrological regime of the region is vulnerable to climatic variations, especially precipitation …
hydrological regime of the region is vulnerable to climatic variations, especially precipitation …
The East River, Colorado, Watershed: A mountainous community testbed for improving predictive understanding of multiscale hydrological–biogeochemical dynamics
Core Ideas Development of a 300‐km2 mountainous headwater testbed began in 2016 in
the East River. The testbed can be used to explore how watershed changes impact …
the East River. The testbed can be used to explore how watershed changes impact …
Elevation-dependent warming in global climate model simulations at high spatial resolution
The enhancement of warming rates with elevation, so-called elevation-dependent warming
(EDW), is one of the regional, still not completely understood, expressions of global …
(EDW), is one of the regional, still not completely understood, expressions of global …
Water vapor and lapse rate feedbacks in the climate system
R Colman, BJ Soden - Reviews of Modern Physics, 2021 - APS
Water vapor is a greenhouse gas that dominates Earth's terrestrial radiation absorption. As
the planetary temperature warms, forced by increasing CO 2 and other greenhouse gases …
the planetary temperature warms, forced by increasing CO 2 and other greenhouse gases …
[HTML][HTML] Climate change in the High Mountain Asia in CMIP6
Abstract Climate change over High Mountain Asia (HMA, including the Tibetan Plateau) is
investigated over the period 1979–2014 and in future projections following the four Shared …
investigated over the period 1979–2014 and in future projections following the four Shared …