Literature DB >> 30743829

Modelling glacier variation and its impact on water resource in the Urumqi Glacier No. 1 in Central Asia.

Hongkai Gao1, Hong Li2, Zheng Duan3, Ze Ren4, Xiaoyu Meng5, Xicai Pan6.   

Abstract

Climate warming is expected to accelerate glacier retreat and shift hydrological regime, which poses great threat to regional water resources in terms of amount, variability, and quality. This is especially true in arid regions with glaciers such as the Central Asia. However, few models manage to mimic both glacier runoff and surface changes with adequate performance. To narrow this gap, we integrated a spatially distributed hydrological model (FLEXG) and a glacier retreat model (∆h-parameterization), and tested the new model in the Urumqi Glacier No. 1 catchment, which is best monitored in China. The model inputs include climate forcing, topographic map and initial ice thickness. Here we validated the model with runoff observation at downstream and glacier measurements, i.e. three historical glacier area maps (1980, 1994 and 2002), annual glacier mass balance (GMB) and equilibrium line altitude (ELA). Results show that the FLEXG-∆h model performed well in estimating runoff (with Kling-Gupta efficiency 0.75 for hydrograph) and reproducing historical glacier area variation. Additionally the model generated reasonably spatial distribution of glacier thickness, which is important to examine glacier evolution at the Urumqi Glacier No. 1. Subsequently we ran the model forced by 12 combinations of two climate scenarios and six bias correction methods to assess the impact of climate change on glacier thinning, retreat, and its influence on water resource. The impact assessment shows that glacier area will lose up to a half (54%) of their 1980 extent in 2050, and up to 80% in 2100; while ice volume will decrease up to 79% in 2050, and 92% in 2100. The tipping point (peak water) of glacier melt supply was projected to occur around 2020 and then runoff would decrease significantly. These results alert us that there is a need for immediate mitigation measures to adapt to fast glacier change to assure long-term water security in this region.
Copyright © 2018. Published by Elsevier B.V.

Entities:  

Keywords:  China; Climate change; FLEX hydrological model; Glacier retreat model; The Urumqi Glacier No. 1 catchment; Water resources

Year:  2018        PMID: 30743829     DOI: 10.1016/j.scitotenv.2018.07.004

Source DB:  PubMed          Journal:  Sci Total Environ        ISSN: 0048-9697            Impact factor:   7.963


  3 in total

1.  Ecological networks reveal contrasting patterns of bacterial and fungal communities in glacier-fed streams in Central Asia.

Authors:  Ze Ren; Hongkai Gao
Journal:  PeerJ       Date:  2019-09-17       Impact factor: 2.984

2.  A surrogate weighted mean ensemble method to reduce the uncertainty at a regional scale for the calculation of potential evapotranspiration.

Authors:  Byoung Hyun Yoo; Junhwan Kim; Byun-Woo Lee; Gerrit Hoogenboom; Kwang Soo Kim
Journal:  Sci Rep       Date:  2020-01-21       Impact factor: 4.379

3.  Bacterial communities in surface and basal ice of a glacier terminus in the headwaters of Yangtze River on the Qinghai-Tibet Plateau.

Authors:  Ze Ren; Hongkai Gao; Wei Luo; James J Elser
Journal:  Environ Microbiome       Date:  2022-03-26
  3 in total

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