img

Wechat

  • CN 62-1070/P
  • ISSN 1000-694X
  • Bimonthly 1981
Adv search

Evaluation on Modeling of Land-Atmosphere Interaction in the Northern Marginal Zone of Taklimakan Desert with CoLM and Correction

  • Jin Lili ,
  • Li Zhenjie ,
  • He Qing ,
  • Liu Yongqiang ,
  • Ali Mamtimin ,
  • Xin Yu
Expand
  • 1. Taklimakan Desert Meteorology Field Experiment Station of CMA, Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China;
    2. Lincang Meteorological Bureau, Lincang 677099, Yunnan, China;
    3. College of Resources & Environmental Science/Ministry of Education Key Laboratory of Oasis Ecology, Xinjiang University, Urumqi 830046, China

Received date: 2017-08-31

  Revised date: 2018-01-25

  Online published: 2018-12-05

Abstract

In this study, observation data during 22 March to 26 July, 2011 were used to simulate the land-atmosphere flux and test the sensitivity of simulation by different surface land parameters, such as surface albedo(α), surface emissivity(ε), aerodynamic roughness length(z0m), thermal roughness length(z0h) and zero plane displacement(d). Sensitivity tests indicate that sensible heat flux(H) and soil temperature(Tg) are sensitive toα, z0m, ε but d. The study site representes the desert underlying surface of the northern marginal zone of the Taklimakan Desert with shifting sand dunes. CoLM model can simulate the average variation of net radiation (Rn), soil heat flux(G0), sensible heat flux(H) and surface soil temperate(Tg). Only in the peak values and peak time of diurnal variation are not ideal. However, CoLM model on soil moisture perform poor. Furthermore, the statistical errors Bias, SEE, NSEE of Rn, H, Tg decreased according to the improved model, particularly. In particular, the statistical errors SEE of Rn decreased 4.21% than default model; the statistical errors Bias of H decreased 25.19% than default model; the statistical errors Bias, SEE and NSEE of Tg decreased 33.33%, 10.45% and 25%.

Cite this article

Jin Lili , Li Zhenjie , He Qing , Liu Yongqiang , Ali Mamtimin , Xin Yu . Evaluation on Modeling of Land-Atmosphere Interaction in the Northern Marginal Zone of Taklimakan Desert with CoLM and Correction[J]. Journal of Desert Research, 2018 , 38(6) : 1287 -1302 . DOI: 10.7522/j.issn.1000-694X.2018.00004

References

[1] Lawford R G.A midterm report on the GEWEX Continental-Scale International Project(GCIP)[J].Journal of Geophysical Research,1999,104(D16):19279-19292.
[2] Gao Z Q,Wang J M,Ma Y M.Calculation of near-surface layer turbulent transport and analysis of surface thermal equilibrium features in Nagqu of Tibet[J].Physics and Chemistry of the Earth,Part B:Hydrology,Oceans and Atmosphere,2000,25(2):135-139.
[3] Gao Z Q,Wang J M,Ma Y M.Study of roughness lengths and drag coefficients over nansha sea region,gobi,desert,oasis and Tibetan Plateau[J].Physics and Chemistry of the Earth,Part B:Hydrology,Oceans and Atmosphere,2000,25(2):141-145.
[4] Gao Z Q,Chae N,Kim J,et al.Modeling of surface energy partitioning,surface temperature,and soil wetness in the Tibetan prairie using the Simple Biosphere Model 2(SiB2)[J].Journal of Geophysical Research,2004,109:D06102.
[5] Wang J,Kim J,Liou Y,et al.Energy balance analysis and one-dimensional simulation of land surface process in a short-grass site of Central Tibetan Plateau[C]//Proceedings of the 1st International Workshop on GAME-Tibet.1999:73-76
[6] Kim J,Choi T,Lee H,et al.Energy partitioning and its imbalance over a prairie site in central Tibetan plateau during GAPE-IOP,1998[J].Eos,Transactions American Geophysical Union,2000,81(22):5-6.
[7] Kim J,Hong J,Gao Z,et al.Can we close the surface energy budget in the Tibetan Plateau[C]//Second Session of International Workshop on TIPEX-GAME/Tibet.2000:13-16.
[8] Tanaka K,Ishikawa H,Hayashi T,et al.Surface energy budget at Amdo on the Tibetan Plateau using GAME/Tibet IOP98 data[J].Journal of the Meteorological Society of Janpan,2001,79(1B):505-517.
[9] Choi T,Hong J,Kim J,et al.Turbulent exchange of heat,water vapor,and momentum over a Tibetan prairie by eddy covariance and flux variance measurements[J].Journal of Geophysical Research,2004,109:D21106.
[10] Hutjes R W A,Kabat P,Running S W,et al.Biospheric aspects of the hydrological cycle[J].Journal of Hydrology,1998,212:1-21.
[11] Benitez P,McCallum L,Obersteiner M,et al.Global supply for carbon sequestration:identifying 2004 Chahine MT.GEWEX:the global energy and water cycle experiment[J].Eos,Transactions American Geophysical Union,1992,73(2):9-14.
[12] Leese J,Jackson T,Pitman A,et al.Meeting summary:GEWEX/BAHC international workshop on soil moisture monitoring,analysis,and prediction for hydrometeorological and hydroclimatological applications[J].Bulletin of the American Meteorological Society,2001,82(7):1423-1430.
[13] Beljaars A C M,Holtslag A A M.Flux parameterization over land surfaces for atmospheric models[J].Journal of Applied Meteorology,1991,30(3):327-341.
[14] Sellers P J,Mintz Y,Sud Y C,et al.A simple biosphere model(SiB) for use within general circulation models[J].Journal of Atmospheric Science,1986,43(6):505-531.
[15] Charney J G.Dynamics of deserts and drought in the Sahel[J].Quarterly Journal of the Royal Meteorological Society,1975,101(428):193-202.
[16] Sud Y C,Smith W E.The influence of surface roughness of deserts on the July circulation[J].Boundary-Layer Meteorology,1985,33(1):15-49.
[17] Sud Y C,Smith W E.Influence of local land surface process on the Indian monsoon-A numerical study[J].Journal of Applied Meteorological,1985,24(10):1015-1036.
[18] Peters-Lidard C D,Blackburn E,Liang X,et al.The effect of soil thermal conductivity parameterization on surface energy fluxes and temperature[J].Journal of Atmospheric Science,1998,55:1029-1224.
[19] Yasunari T.Role of land-atmosphere interaction on Asian monsoon climate[J].Journal of the Meteorological Society of Japan,2007,85B:55-75.
[20] Twine T E,Kucharik C J,Foley J A.Effects of land cover change on the energy and water balance of the Mississippi River basin[J].Journal of Hydrometeorology,2004,5(4):640-655.
[21] 符淙斌,袁慧玲.恢复自然植被对东亚夏季气候和环境影响的一个虚拟试验[J].科学通报,2001,46(8):691-695.
[22] Gao X J,Luo Y,Lin W T,et al.Simulation of effects of land use change on climate in China by a regional climate model[J].Advances in Atmospheric Sciences,2003,20(4):583-592.
[23] 马迪,吕世华,鲍艳,等.沙漠下垫面地面温度及能量收支的BATS模式参数化改进[J].中国沙漠,2017,37(4):749-754.
[24] 丁一汇,李巧萍,董文杰.植被变化对中国区域气候影响的数值模拟研究[J].气象学报,2005,63(5):613-621.
[25] 曹丽娟,张冬峰,张勇,等.中国当代土地利用变化对黄河流域径流影响[J].大气科学,2008,32(2):300-308.
[26] Webb E K,Pearman G I,Leuning R.Correction of flux measurements for density effects due to heat and water vapor transfer[J].Quarterly Journal of the Royal Meteorological Society,1980,106(447):85-100.
[27] 宋耀明,郭维栋,张耀存.陆面过程模式CoLM和NCAR_CLM3.0对中国典型森林生态系统陆气相互作用的模拟Ⅱ.不同参数化方案对模拟结果的影响[J].气候与环境研究,2009,14(3):243-257.
[28] 郑婧,谢正辉,戴永久,等.陆面过程模型CoLM与区域气候模式RegCM3的耦合及初步评估[J].大气科学,2009,33(4):737.
[29] 刘黎平,钱永甫.区域模式和GCM对青藏高原和西北地区气候模拟结果的对比分析[J].高原气象,2000,19(3):313-322.
[30] 塔依尔,吕新,马兰花,等.古尔班通古特沙漠南缘绿洲净辐射及其热量通量的变化研究[J].石河子大学学报:自然科学版,2005,23(5):587-590.
[31] 魏文寿,董光荣.古尔班通古特沙漠的辐射热量交换分析[J].中国沙漠,1997,17(4):335-341.
[32] Li W P,Chineke T C,Liu X,et al.Atmospheric diabatic heating and summertime circulation in Asia-Africa area[J].Advances in Atmospheric Sciences,2001,18(2):257-269.
[33] 王敏仲,魏文寿,杨莲梅,等.塔克拉玛干沙漠地表潜热时空特征分析[J].中国沙漠,2008,28(5):940-947.
[34] 王敏仲,杨莲梅,魏文寿,等.塔克拉玛干沙漠地表感热特征分析[J].干旱区资源与环境,2009,23(5):172-178.
[35] 何清,赵景峰.塔里木盆地浮尘时空分布及对环境影响的研究[J].中国沙漠,1997,17(2):119-126.
[36] Liu Y Q,He Q,Zhang H S,et al.Improving the CoLM in Taklimakan Desert Hinterland with accurate key parameters and an appropriate parameterization scheme[J].Advances in Atmospheric Sciences,2012,29(2):381-390.
[37] 刘永强,艾力·买买提明,何清.对陆面过程模型CoLM中关键参数的修正[J].干旱区研究,2014,31(4):611-618.
[38] Wang X M,Dong Z B,Zhang J W,et al.Geomorphology of sand dunes in the Northeast Taklimakan Desert[J].Geomorphology,2002,42(3/4):183-195.
[39] Sun J M,Liu T S.The age of the Taklimakan Desert[J].Science,2006,312(5780):1621.
[40] 钱正安,宋敏红,李万元.近50年来中国北方沙尘暴的分布及变化趋势分析[J].中国沙漠,2002,22(2):106-111.
[41] 托马斯T沃纳.沙漠气象学[M].魏文寿等,译.北京:气象出版社,2008:197.
[42] Dickinson R E,Kennedy P J,Henderson-Sellers A.Biosphere-atmosphere transfer scheme(BATS) version 1e as coupled to the NCAR community climate model[R].NCAR Tech.,Note NCAR/TN-387+STR.,1993:72.
[43] Colello G D,Grivet C,Sellers P J,et al.Modeling of energy,water,and CO2 flux in a temperate grassland ecosystem with SiB2:May-October 1987[J].Journal of Atmosphere Science,1998,55(7):1141-1169.
[44] Yang K,Koike T,Ishikawa H,et al.Turbulent flux transfer over bare-soil surfaces:characteristics and parameterization[J].Journal of Applied Meteorology & Climatology,2008,47(1):276-290.
[45] 阳坤,王介民.一种基于土壤温湿度资料计算地表土壤热通量的温度预报校正法[J].中国科学D辑:地球科学,2008,38(2):243-250.
[46] Kanda M,Kanega M,Kawai T,et al.Roughness lengths for momentum and heat derived from outdoor urban scale models[J].Journal of Applied Meteorology & Climatology,2007,46(7):1067-1079.
[47] Owen P R,Thomson W R.Heat transfer across rough surfaces[J].Journal of Fluid Mechanics,1963,15(3):321-334.
[48] Chamberlain A C.Transport of gases to and from surfaces with bluff and wave-like roughness elements.Quart[J].Quarterly Journal of the Royal Meteorological Society,1968,94(401):318-332.
[49] Zeng X B,Dickinson R E.Effect of surface sublayer on surface skin temperature and fluxes[J].Journal of Climate,1998,11(4):537-550.
[50] Dai Y J,Zeng X B,Dickinson R E.Common Land Model(CLM)(Technical Documentation and User's Guide)[Z].Atlanta,USA:Georgia Institute of Technology,2001.
[51] 房云龙,孙菽芬,李倩,等.干旱区陆面过程模型参数优化和地气相互作用特征的模拟研究[J].大气科学,2010,34(2):290-306.
[52] 张瑞军,何清,孔丹,等.塔克拉玛干沙漠北缘沙尘暴源区地表沉积物粒度特征[J].干旱区研究,2008,25(6):887-893.
[53] 李振山,陈广庭,冯起,等.塔克拉玛干沙漠腹地纵向沙垄表面沙物质粒度特征[J].干旱区资源与环境,1998,12(1):21-28.
[54] 张宇,吕世华.陆面过程模式对不同土壤物理性质的敏感性研究[J].冰川冻土,2001,23(3):270-275.
[55] 吴龙刚,王爱慧,盛炎平.土壤质地对中国区域陆面过程模拟的影响[J].气候与环境研究,2014,19(5):559-571.
Outlines

/