Decoupling of warming mountain snowpacks from hydrological regimes
Climate warming will reduce the duration of mountain snowpacks and spring runoff, impacting the timing, volume, reliability, and sources of water supplies to mountain headwaters of rivers that support a large proportion of humanity. It is often assumed that snow hydrology will change in proportion t...
Main Authors: | J I López-Moreno, J W Pomeroy, E Alonso-González, E Morán-Tejeda, J Revuelto |
---|---|
Format: | Article |
Language: | English |
Published: |
IOP Publishing
2020-01-01
|
Series: | Environmental Research Letters |
Subjects: | |
Online Access: | https://doi.org/10.1088/1748-9326/abb55f |
Similar Items
-
Changes in the frequency of global high mountain rain-on-snow events due to climate warming
by: J I López-Moreno, et al.
Published: (2021-01-01) -
Different sensitivities of snowpacks to warming in Mediterranean climate mountain areas
by: J I López-Moreno, et al.
Published: (2017-01-01) -
Testing the recent snow drought as an analog for climate warming sensitivity of Cascades snowpacks
by: Matthew G Cooper, et al.
Published: (2016-01-01) -
The Role of Basin Geometry in Mountain Snowpack Responses to Climate Change
by: Joseph M. Shea, et al.
Published: (2021-02-01) -
Snowpack variations and their hazardous effects under climate warming in the central Tianshan Mountains
by: Jian-Sheng Hao, et al.
Published: (2024-06-01)