A Test Study of an Energy and Mass Balance Model Application to a Site on Urumqi Glacier No. 1, Chinese Tian Shan

In this study, energy and mass balance is quantified using an energy balance model to represent the glacier melt of Urumqi Glacier No. 1, Chinese Tian Shan. Based on data from an Automatic Weather Station (4025 m a.s.l) and the mass balance field survey data nearby on the East Branch of the glacier,...

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Main Authors: Puyu Wang, Zhongqin Li, Christoph Schneider, Hongliang Li, Alexandra Hamm, Shuang Jin, Chunhai Xu, Huilin Li, Xiaoying Yue, Min Yang
Format: Article
Language:English
Published: MDPI AG 2020-10-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/12/10/2865
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author Puyu Wang
Zhongqin Li
Christoph Schneider
Hongliang Li
Alexandra Hamm
Shuang Jin
Chunhai Xu
Huilin Li
Xiaoying Yue
Min Yang
author_facet Puyu Wang
Zhongqin Li
Christoph Schneider
Hongliang Li
Alexandra Hamm
Shuang Jin
Chunhai Xu
Huilin Li
Xiaoying Yue
Min Yang
author_sort Puyu Wang
collection DOAJ
description In this study, energy and mass balance is quantified using an energy balance model to represent the glacier melt of Urumqi Glacier No. 1, Chinese Tian Shan. Based on data from an Automatic Weather Station (4025 m a.s.l) and the mass balance field survey data nearby on the East Branch of the glacier, the “COupled Snowpack and Ice surface energy and Mass balance model” (COSIMA) was used to derive energy and mass balance simulations during the ablation season of 2018. Results show that the modeled cumulative mass balance (−0.67 ± 0.03 m w.e.) agrees well with the in-situ measurements (−0.64 ± 0.16 m w.e.) (r<sup>2</sup> = 0.96) with the relative difference within 5% during the study period. The correlation coefficient between modeled and observed surface temperatures is 0.88 for daily means. The main source of melt energy at the glacier surface is net shortwave radiation (84%) and sensible heat flux (16%). The energy expenditures are from net longwave radiation (55%), heat flux for snow/ice melting (32%), latent heat flux of sublimation and evaporation (7%), and subsurface heat flux (6%). The sensitivity testing of mass balance shows that mass balance is more sensitive to temperature increase and precipitation decrease than temperature decrease and precipitation increase.
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spelling doaj.art-c6b0433e8a644e5295426b43ebc25b2a2023-11-20T17:11:59ZengMDPI AGWater2073-44412020-10-011210286510.3390/w12102865A Test Study of an Energy and Mass Balance Model Application to a Site on Urumqi Glacier No. 1, Chinese Tian ShanPuyu Wang0Zhongqin Li1Christoph Schneider2Hongliang Li3Alexandra Hamm4Shuang Jin5Chunhai Xu6Huilin Li7Xiaoying Yue8Min Yang9State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaState Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaGeography Department/Geographisches Institute, Humboldt-Universität zu Berlin, D-10099 Berlin, GermanyState Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaGeography Department/Geographisches Institute, Humboldt-Universität zu Berlin, D-10099 Berlin, GermanyState Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaState Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaState Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaState Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaState Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaIn this study, energy and mass balance is quantified using an energy balance model to represent the glacier melt of Urumqi Glacier No. 1, Chinese Tian Shan. Based on data from an Automatic Weather Station (4025 m a.s.l) and the mass balance field survey data nearby on the East Branch of the glacier, the “COupled Snowpack and Ice surface energy and Mass balance model” (COSIMA) was used to derive energy and mass balance simulations during the ablation season of 2018. Results show that the modeled cumulative mass balance (−0.67 ± 0.03 m w.e.) agrees well with the in-situ measurements (−0.64 ± 0.16 m w.e.) (r<sup>2</sup> = 0.96) with the relative difference within 5% during the study period. The correlation coefficient between modeled and observed surface temperatures is 0.88 for daily means. The main source of melt energy at the glacier surface is net shortwave radiation (84%) and sensible heat flux (16%). The energy expenditures are from net longwave radiation (55%), heat flux for snow/ice melting (32%), latent heat flux of sublimation and evaporation (7%), and subsurface heat flux (6%). The sensitivity testing of mass balance shows that mass balance is more sensitive to temperature increase and precipitation decrease than temperature decrease and precipitation increase.https://www.mdpi.com/2073-4441/12/10/2865glacier ablationenergy balancemass balanceUrumqi Glacier No. 1Chinese Tian Shan
spellingShingle Puyu Wang
Zhongqin Li
Christoph Schneider
Hongliang Li
Alexandra Hamm
Shuang Jin
Chunhai Xu
Huilin Li
Xiaoying Yue
Min Yang
A Test Study of an Energy and Mass Balance Model Application to a Site on Urumqi Glacier No. 1, Chinese Tian Shan
Water
glacier ablation
energy balance
mass balance
Urumqi Glacier No. 1
Chinese Tian Shan
title A Test Study of an Energy and Mass Balance Model Application to a Site on Urumqi Glacier No. 1, Chinese Tian Shan
title_full A Test Study of an Energy and Mass Balance Model Application to a Site on Urumqi Glacier No. 1, Chinese Tian Shan
title_fullStr A Test Study of an Energy and Mass Balance Model Application to a Site on Urumqi Glacier No. 1, Chinese Tian Shan
title_full_unstemmed A Test Study of an Energy and Mass Balance Model Application to a Site on Urumqi Glacier No. 1, Chinese Tian Shan
title_short A Test Study of an Energy and Mass Balance Model Application to a Site on Urumqi Glacier No. 1, Chinese Tian Shan
title_sort test study of an energy and mass balance model application to a site on urumqi glacier no 1 chinese tian shan
topic glacier ablation
energy balance
mass balance
Urumqi Glacier No. 1
Chinese Tian Shan
url https://www.mdpi.com/2073-4441/12/10/2865
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