Evaluating and Improving the Performance of Three 1-D Lake Models in a Large Deep Lake of the Central Tibetan Plateau
文献类型:期刊论文
作者 | Huang, Anning1; Lazhu2; Wang, Junbo2; Dai, Yongjiu3; Yang, Kun4; Wei, Nan3; Wen, Lijuan5; Wu, Yang6,7; Zhu, Xueyan1; Zhang, Xindan1 |
刊名 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES |
出版日期 | 2019-03-27 |
卷号 | 124期号:6页码:3143-3167 |
ISSN号 | 2169-897X |
关键词 | lake model evaluation Lake Nam Co Tibetan Plateau thermal structure |
DOI | 10.1029/2018JD029610 |
通讯作者 | Lazhu(lazhu@itpcas.ac.cn) |
英文摘要 | The ability of FLake, WRF-Lake, and CoLM-Lake models in simulating the thermal features of Lake Nam Co in Central Tibetan Plateau has been evaluated in this study. All the three models with default settings exhibited distinct errors in the simulated vertical temperature profile. Then model calibration was conducted by adjusting three (four) key parameters within FLake and CoLM-Lake (WRF-Lake) in a series of sensitive experiments. Results showed that each model's performance is sensitive to the key parameters and becomes much better when adjusting all the key parameters relative to tuning single parameter. Overall, setting the temperature of maximum water density to 1.1 degrees C instead of 4 degrees C in the three models consistently leads to improved vertical thermal structure simulation during cold seasons; reducing the light extinction coefficient in FLake results in much deeper mixed layer and warmer thermocline during warm seasons in better agreement with the observation. The vertical thermal structure can be clearly improved by decreasing the light extinction coefficient and increasing the turbulent mixing in WRF-Lake and CoLM-Lake during warm seasons. Meanwhile, the modeled water temperature profile in warm seasons can be significantly improved by further replacing the constant surface roughness lengths by a parameterized scheme in WRF-Lake. Further intercomparison indicates that among the three calibrated models, FLake (WRF-Lake) performs the best to simulate the temporal evolution and intensity of temperature in the layers shallower (deeper) than 10m, while WRF-Lake is the best at simulating the amplitude and pattern of the temperature variability at all depths. |
收录类别 | SCI |
WOS关键词 | REGIONAL CLIMATE MODEL ; LAURENTIAN GREAT-LAKES ; NAM CO BASIN ; SHALLOW LAKE ; FLAKE MODEL ; POTENTIAL TEMPERATURE ; SUMMER PRECIPITATION ; WATER TEMPERATURE ; PHYSICAL CONTROLS ; DIFFUSE FRACTION |
WOS研究方向 | Meteorology & Atmospheric Sciences |
WOS类目 | Meteorology & Atmospheric Sciences |
语种 | 英语 |
出版者 | AMER GEOPHYSICAL UNION |
WOS记录号 | WOS:000464653500018 |
URI标识 | http://www.irgrid.ac.cn/handle/1471x/2555501 |
专题 | 寒区旱区环境与工程研究所 |
通讯作者 | Lazhu |
作者单位 | 1.Nanjing Univ, Sch Atmospher Sci, CMA NJU Joint Lab Climate Predict Studies, Nanjing, Jiangsu, Peoples R China 2.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing, Peoples R China 3.Sun Yat Sen Univ, Sch Atmospher Sci, Guangdong Prov Key Lab Climate Change & Nat Disas, Guangzhou, Guangdong, Peoples R China 4.Tsinghua Univ, Dept Earth Syst Sci, Beijing, Peoples R China 5.Chinese Acad Sci, Key Lab Land Surface Proc & Climate Change Cold &, Lanzhou, Gansu, Peoples R China 6.Nanjing Univ, Sch Atmospher Sci, State Key Lab State Severe Weather, Nanjing, Jiangsu, Peoples R China 7.Nanjing Univ, Sch Atmospher Sci, Joint Ctr Atmospher Radar Res CMA NJU, Nanjing, Jiangsu, Peoples R China |
推荐引用方式 GB/T 7714 | Huang, Anning,Lazhu,Wang, Junbo,et al. Evaluating and Improving the Performance of Three 1-D Lake Models in a Large Deep Lake of the Central Tibetan Plateau[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2019,124(6):3143-3167. |
APA | Huang, Anning.,Lazhu.,Wang, Junbo.,Dai, Yongjiu.,Yang, Kun.,...&Cai, Shuxin.(2019).Evaluating and Improving the Performance of Three 1-D Lake Models in a Large Deep Lake of the Central Tibetan Plateau.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,124(6),3143-3167. |
MLA | Huang, Anning,et al."Evaluating and Improving the Performance of Three 1-D Lake Models in a Large Deep Lake of the Central Tibetan Plateau".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 124.6(2019):3143-3167. |
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来源:寒区旱区环境与工程研究所
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