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DOI | 10.1029/2020JD033105 |
Long-Term Temporal Scale-Dependent Warming Effects on the Mass Balance in the Dongkemadi Glacier, Tibetan Plateau | |
Liang, Liqiao; Cuo, Lan; Liu, Qiang | |
通讯作者 | Liang, LQ (通讯作者) |
发表日期 | 2020 |
ISSN | 2169-897X |
EISSN | 2169-8996 |
卷号 | 125期号:20 |
英文摘要 | Understanding how climate change impacts glaciers is important in predicting their prospective response and crucial in forecasting water supplies and potential influences within surrounding lowland areas. This study evaluated annual, seasonal, and monthly warming effects on the mass balance in the Dongkemadi (DKMD) Glacier throughout 1960-2009. Results showed an increasing trend in annual, seasonal, and monthly scale air temperature variation: high during the cool season (0.0347 degrees C a(-1)) and low during the warm season (0.0222 degrees C a(-1)). Warming rates variability effects at all three scales were roughly the same. Seasonal and monthly warming rates produced roughly the same effect on glacier mass balance, while the annual warming rate overestimated annual mass balance by 20.0%. July produced the largest monthly warming effect overestimation at an annual warming rate (11.9 mm w.e.; 29.3%), followed by August and June. Furthermore, increases in annual melt energy (approximately 70%) throughout the study period primarily resulted from increases in net radiation and turbulent heat flux, which mainly occurred during the warm season (>96%). Proportional increases in warming-induced rainfall caused a decrease in mass balance while contributing to differing warming rate effects through reductions in mass inputs and albedo rather than through increases in rain-induced heat flux. Results confirmed the effectiveness of using seasonal scale warming rates to investigate warming effects on glacier and meltwater changes in the Dongkemadi Glacier. This study provides valuable information to accurately evaluate warming effects on energy/mass balance of glaciers worldwide. |
关键词 | CLIMATE-CHANGEHYDROLOGICAL CYCLERUNOFF CHANGESTEMPERATURESENSITIVITIESVARIABILITYRADIATIONHUMIDITYPATTERNSIMPACTS |
英文关键词 | warming effects; timescales; glacier mass balance; glacier energy balance; glacier modeling; Tibetan Plateau |
语种 | 英语 |
WOS研究方向 | Meteorology & Atmospheric Sciences |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS记录号 | WOS:000588398800014 |
来源期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
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来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/259809 |
推荐引用方式 GB/T 7714 | Liang, Liqiao,Cuo, Lan,Liu, Qiang. Long-Term Temporal Scale-Dependent Warming Effects on the Mass Balance in the Dongkemadi Glacier, Tibetan Plateau[J]. 中国科学院青藏高原研究所,2020,125(20). |
APA | Liang, Liqiao,Cuo, Lan,&Liu, Qiang.(2020).Long-Term Temporal Scale-Dependent Warming Effects on the Mass Balance in the Dongkemadi Glacier, Tibetan Plateau.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,125(20). |
MLA | Liang, Liqiao,et al."Long-Term Temporal Scale-Dependent Warming Effects on the Mass Balance in the Dongkemadi Glacier, Tibetan Plateau".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 125.20(2020). |
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