塔克拉玛干沙漠北缘夏秋冬季地表能量平衡闭合特征

doi:10.13866/j.azr.2018.04.10

干旱区研究 ›› 2018, Vol. 35 ›› Issue (4): 821-829.doi: 10.13866/j.azr.2018.04.10

塔克拉玛干沙漠北缘夏秋冬季地表能量平衡闭合特征

曹寰琦^1,2,3，何清^2,3，金莉莉^2,3，李振杰⁴，杨兴华^2,3，霍文^2,3

(1.新疆大学资源与环境科学学院,新疆乌鲁木齐 830046；2.中国气象局乌鲁木齐沙漠气象研究所,新疆乌鲁木齐 830002；3.新疆塔克拉玛干沙漠大气环境观测试验站,新疆塔中 841000；4.云南省临沧市气象局,云南临沧 677099)

收稿日期:2017-05-24 修回日期:2017-12-13 出版日期:2018-07-15 发布日期:2018-07-19
作者简介:曹寰琦（1992—），女，硕士研究生，主要从事沙漠气象研究. E-mail:caohuanqi821@qq.com
基金资助:
国家自然科学基金项目（41605008），中央级公益性科研院所基本科研业务费专项资金（IDM201505）；公益性行业（气象）科研专项[GYHY(QX)201506001-14]

Surface Energy Balance Closure of Summer,Autumn and Winter in the Northern Margin of Taklimakan Desert

CAO Huan-qi^{1, 2, 3}, HE Qing^{2, 3}, JIN Li-li^{2, 3}, LI Zhen-jie⁴, YANG Xing-hua^{2, 3}, HUO Wen^{2, 3}

(1. College of Resources and Environmental Sciences, Xinjiang University, Urumqi 830046,China;2. Institute Desert Meteorology, China Meteorological Administration, Urumqi 830002, China;3. Taklimakan Desert Atmosphere and Environment Observation and Experimental Station, Tazhong 841000, Xinjiang, China;4. Lincang Meteorological Office, Lincang 677099, Yunnan Province, China)

Received:2017-05-24 Revised:2017-12-13 Published:2018-07-15 Online:2018-07-19

摘要/Abstract

摘要： 利用塔克拉玛干沙漠北缘肖塘陆—气相互作用观测站2014年7月—12月的陆面通量数据，通过最小二乘法（OLS）和能量平衡比率法（EBR）研究该地区能量平衡闭合特征。结果表明：能量通量各分量均呈倒“U”形单峰变化趋势，除潜热通量外，均有明显的季节变化特征，表现为：夏季＞秋季＞冬季。能量平衡闭合程度：全天＞白天＞夜间，且具有逐月递减的变化趋势。地表以下5cm处土壤热通量下的能量闭合程度明显高于地表土壤热通量下的能量闭合程度。能量闭合率在日出日落时段波动剧烈，夜间为负，且下午明显高于上午。不同天气下的能量闭合程度表现为：晴天＞阴天＞沙尘暴＞降雨。

Abstract: Energy balance in the terrestrial ecosystem plays an important role in regional climate and water balance. In this study, the characteristics of surface energy balance were researched using the ordinary least square (OLS) method and energy balance ratio (EBR) method based on the surface flux data observed at Xiaotang land-atmospheric interation observation station in the northern marginal zone of the Taklimakan Desert during the period from July to December 2014. The results showed that, except for the latent heat flux, the daily variation curves of other energy flux components were inverted “U-shaped” and unimodal, which were characterized by seasonal variation and in an order of summer > autumn > winter. The energy balance was in an order of whole day > daytime > night and in a degressive trend. The energy closure degree of 5 cm deep soil heat flux was significantly higher than that of topsoil heat flux. The energy closure ratio fluctuated sharply at the sunrise and sunset, it was negative at night, and apparently higher in the afternoon than in the morning. Under the different weather conditions, the energy closure ratio was in an order of sunshine day > cloudy day > sandstorm day > rainfall day.

Key words: eddy covariance, energy balance closure, energy balance ratio, ordinary least square, Taklimakan Desert

曹寰琦, 何清, 金莉莉, 李振杰, 杨兴华, 霍文. 塔克拉玛干沙漠北缘夏秋冬季地表能量平衡闭合特征[J]. 干旱区研究, 2018, 35(4): 821-829.

CAO Huan-qi, HE Qing, JIN Li-li, LI Zhen-jie, YANG Xing-hua, HUO Wen. Surface Energy Balance Closure of Summer,Autumn and Winter in the Northern Margin of Taklimakan Desert[J]. Arid Zone Research, 2018, 35(4): 821-829.

参考文献

[1]陈琛.淮河流域农田生态系统能量平衡与闭合研究[D].合肥:安徽农业大学,2012.[Chen Chen.Observational Study of Surface Energy Balance and Energy Closure in the Farmland Ecosystems in Huaihe River Basin[D].Hefei:Anhui Agricultural University,2012.]
[2]杨启东,左洪超,杨扬等.近地层能量闭合度对陆面过程模式影响[J].地球物理学报,2012,55(9):2876-2888.[Yang Qidong,Zuo Hongchao,Yang Yang,et al.On the effect of the near-surface layer energy closure degree on the land surface process simulations[J].Chinese Journal of Geophys,2012,55(9):2876-2888.]
[3] Heusinkveld B G, Jacobs A F G, Holtslag A A M, et al. Surface energy balance closure in an arid region: role of soil heat flux[J]. Agricultural and Forest Meteorology, 2004, 122(1/2): 21-37.
[4] Gao Z. Determination of soil heat flux in a Tibetan short-grass prairie[J]. Boundary-Layer Meteorology, 2005, 114(1): 165-178.
[5]王介民,王维真,刘绍民,等.近地层能量平衡闭合问题—综述及个例分析[J].地球科学进展,2009,24(7):705-713.[Wang Jiemin,Wang Weizhen,Liu Shaomin,et al.The problems of surface energy balance closure：An overview and case study[J].Advances in Earth Science,2009,24(7):705-713.]
[6] Wilson K, Goldstein A, Falge E, et al. Energy balance closure at FLUXNET sites[J]. Agricultural and Forest Meteorology, 2002, 113(1): 223-243.
[7] Stoy P C, Mauder M, Foken T, et al. A data-driven analysis of energy balance closure across FLUXNET research sites: The role of landscape scale heterogeneity[J]. Agricultural and forest meteorology, 2013, 171: 137-152.
[8]李正泉,于贵瑞,温学发,等.中国通量观测网络(ChinaFLUX)能量平衡闭合状况的评价[J].中国科学D辑:地球科学,2004, 34(增刊2): 46-56.[Li Zhengquan,Yu Guirui,Wen Xuefa,et al. Evaluation of the energy balance closure of China FLUX observation network[J]. Scientia Sinica(Terrae),2004,34(Suppl.2) :46-56.]
[9]岳平,张强,牛生杰,等.半干旱草原下垫面能量平衡特征及土壤热通量对能量闭合率的影响[J].气象学报,2012,70(1):136-143.[Yue Ping,Zhang Qiang,Niu Shengjie,et al. Characters of surface energy balance over a semi-arid grassland and effects of soil heat flux on energy balance closure[J]. Acta Meteorologica Sinica , 2012,70(1):136-143.]
[10]张强,李宏宇. 黄土高原地表能量不闭合度与垂直感热平流的关系[J]. 物理学报,2010,59(8):5889-5896. [Zhang Qiang,Li Hongyu. The relationship between surface energy balance unclosure and vertical sensible heat advection over the Loess Plateau[J]. Acta Physica Sinica,2010,59(8):5889-5896.]
[11] Yue P, Li Y, Zhang Q, et al. Surface energy-balance closure in a gully region of the Loess Plateau at SACOL on eastern edge of Tibetan Plateau[J]. Journal of the Meteorological Society of Japan. 2012, 90c: 173-184.
[12]张佩,袁国富,朱治林.荒漠河岸林涡度相关通量测定中平均时间的确定及其对通量计算的影响[J].干旱区地理,2013,36(1):400-408.[Zhang Pei,Yuan Guofu,Zhu Zhilin.Determination of the averaging period of eddy covariance measurement and its influences on the calculation of fluxes in desert riparian forest[J]. Arid Land Geography, 2013,36(1):400-408.]
[13]王延慧,买买提艾力·买买提依明,何清,等.塔克拉玛干沙漠北缘地表能量收支特征[J].沙漠与绿洲气象,2014,8(3):34-41. [WangYanhui, Ali Mamtimin,He Qing,et al. Characteristics of energy budget in the northern margin of the Taklimakan Desert[J]. Desert and Oasis Meteorology,2014,8(3):34-41.]
[14]张文斌,买买提艾力·买买提依明,何清,等.塔克拉玛干沙漠不同区域土壤热通量比较[J].沙漠绿洲与气象,2016,10(2):57-62. [Zhang Wenbin,Ali Mamtimin,He Qing,et al. Comparison of the soil heat flux variations in different areas over the Taklimakan Desert[J]. Desert and Oasis Meteorology,2016,10(2):57-62.]
[15] Yang K, Koike T, Ishikawa H, et al. Turbulent flux transfer over bare-soil surfaces: Characteristics and parameterization[J]. Journal of Applied Meteorology and Climatology, 2008, 47(1): 276-290.
[16]朱治林,孙晓敏,温学友,等.中国通量网(China FLUX)夜间CO2涡度相关通量数据处理方法研究[J].中国科学D辑:地球科学,2006,36(增刊1):34－44.[Zhu Zhilin,Sun Xiaomin,WenXueyou,et al. Study on the related FLUX data processing of China FLUX network nocturnal CO2 vorticity[J]. Scientia Sinica(Terrae),2006,36(Suppl.1):34-44.]
[17]阳坤,王介民.一种基于土壤温湿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.
[Yang Kun,Wang Jiemin. A temperature prediction and correction method based on soil temperature and humidity data is used to calculate the heat flux of surface soil[J]. Scientia Sinica(Terrae),2008,38(2):243-250.]
[18]李泉,张宪洲,石培礼,等.西藏高原高寒草甸能量平衡闭合研究[J].自然资源学报,2008,22(3):391-399.[Li Quan,Zhang Xianzhou,Shi Peili,et al.Study on the energy balance closure of alpine meadow on Tibetan Plateau[J].Journal of Natural Resources,2008, 22(3):391-399.]
[19] 马虹,陈亚宁,李卫红.荒漠河岸柽柳(Tamarix chinensis)灌丛的能量平衡特征[J].中国沙漠,2014,34(1),108-117.[Ma Hong,Chen Yaning,Li Weihong.Characteristics of energy balance of riparian Tamarix shrubs in desert[J].Journal of Desert Research, 2014,34(1): 108-117.]
[20] Foken T. The energy balance closure problem: An overview[J]. Ecological Applications, 2008, 18(6): 1351-1367.
[21]马小红,苏永红,鱼腾飞,等.荒漠河岸胡杨林生态系统涡度相关通量数据处理与质量控制方法研究[J].干旱区地理,2015,38(3):626-635.[Ma Xiaohong,Su Yonghong,Yu Tengfei,et al. Data processing and quality control of eddy covariance in desert riparian forest[J].Arid Land Geography,2015,38(3):626-635.]
[22]杨彦龙,左洪超,赵舒曼,等.夏季晴天沙漠绿洲非均匀下垫面地表能量平衡分析[J].干旱气象,2016,34(3):412-422.[Yang Yanlong，Zuo Hongchao,Zhao Shuman，et al． Analysis of surface energy balance in desert - oasis heterogenous underlying surface in sunny day of Summer[J]．Journal of Arid Meteorology,2016,34( 3) : 412-422.]
[23]岳平,张强,赵文,等.黄土高原地表能量闭合特征及土壤通量参数化[J].冰川冻土,2012,34(3):583-590.[Yue Ping,Zhang Qiang,Zhao Wen,et al. Surface energy –balance closure features and parameterization of soil heat flux on the Loess Plateau[J].Journal of Glaciology and Geocryology, 2012,34(3):583-590.]
[24] 原文文,同小娟,张劲松,等.黄河小浪底人工混交林生长季能量平衡特征.生态学报,2015,35(13):4492-4499.[Yuan Wenwen,Tong Xiaojuan,Zhang Jinsong,et al. Characteristics of energy balance of a mixed plantation in the Xiaolangdi area in the growing season[J].Acta Ecologica Sinica,2015,35( 13) : 4492-4499.]

塔克拉玛干沙漠北缘夏秋冬季地表能量平衡闭合特征

Surface Energy Balance Closure of Summer,Autumn and Winter in the Northern Margin of Taklimakan Desert

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