Articles | Volume 9, issue 3
https://doi.org/10.5194/tc-9-1229-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-9-1229-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Weak precipitation, warm winters and springs impact glaciers of south slopes of Mt. Everest (central Himalaya) in the last 2 decades (1994–2013)
Ev-K2-CNR Committee, Via San Bernardino, 145, Bergamo 24126, Italy
National Research Council, Water Research Institute, Brugherio (IRSA-CNR), Italy
N. Guyennon
National Research Council, Water Research Institute, Roma (IRSA-CNR), Italy
S. Thakuri
Ev-K2-CNR Committee, Via San Bernardino, 145, Bergamo 24126, Italy
National Research Council, Water Research Institute, Brugherio (IRSA-CNR), Italy
G. Viviano
National Research Council, Water Research Institute, Brugherio (IRSA-CNR), Italy
E. Romano
National Research Council, Water Research Institute, Roma (IRSA-CNR), Italy
E. Vuillermoz
Ev-K2-CNR Committee, Via San Bernardino, 145, Bergamo 24126, Italy
P. Cristofanelli
Ev-K2-CNR Committee, Via San Bernardino, 145, Bergamo 24126, Italy
National Research Council, Institute of Atmospheric Sciences and Climate (ISAC-CNR) Bologna, Italy
P. Stocchi
National Research Council, Institute of Atmospheric Sciences and Climate (ISAC-CNR) Bologna, Italy
G. Agrillo
National Research Council, Institute of Atmospheric Sciences and Climate (ISAC-CNR) Bologna, Italy
Y. Ma
Institute of Tibetan Plateau Research, Chinese Academy of Science, Beijing, China
G. Tartari
Ev-K2-CNR Committee, Via San Bernardino, 145, Bergamo 24126, Italy
National Research Council, Water Research Institute, Brugherio (IRSA-CNR), Italy
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Short summary
Climate-trends data in Himalaya are completely absent at high elevation. We explore the south slopes of Mt Everest though time series reconstructed from 7 stations (2660-5600m) during 1994-2013. The main increase in temp is concentrated outside of the monsoon, minimum temp increased far more than maximum, while we note a precipitation weakening. We contribute to change the perspective on which climatic drivers (temperature vs. precipitation) led mainly the glacier responses in the last 20 yr.
Climate-trends data in Himalaya are completely absent at high elevation. We explore the south...