Vol.21, NO.6, 2010
Turn off MathJax
Article Contents
Article Navigation >  Journal of Applied Meteorological Science  > 2010  >  21(6): 649-658
Liao Rongwei, Zhao Ping. Climate characteristics of moisture budget in humid region affected by East Asian monsoon. J Appl Meteor Sci, 2010, 21(6): 649-658.
Citation: Liao Rongwei, Zhao Ping. Climate characteristics of moisture budget in humid region affected by East Asian monsoon. J Appl Meteor Sci, 2010, 21(6): 649-658.
shu

Climate Characteristics of Moisture Budget in Humid Region Affected by East Asian Monsoon

  • 1.

    Chinese Academy of Meteorological Sciences, Beijing 100081

  • 2.

    Graduate University of Chinese Academy of Sciences, Beijing 100049

  • 3.

    National Meteorological Information Centrr, Beijing 100081

  • 4.

    State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081

  • Received Date: 2010-03-29
  • Rev Recd Date: 2010-10-08
  • Publish Date: 2010-12-31
    Abstract
  • Based on 1958—2007 NCEP/NCAR reanalysis data, the characteristics of moisture budget in humid region affected by East Asian Monsoon are calculated by moisture transport, moisture flux divergence and P-E methods. The correlation coefficients of climatological variability calculated by these methods are 0.91, 0.71, 0.81, and the percentage of ε are 17.4%, 44.1% and 44%. The results calculated by moisture transport and moisture flux divergence methods are nearly the same. The results reveal net income of moisture budget thoughout the year especially in spring and summer, while in winter and autumn it's relatively weaker. Using moisture flux divergence and P-E methods, the absolute errors in summer are larger than in other seasons. In spring and summer, water transport and moisture flux divergence are both stronger than those in autumn and winter. For the meridional moisture transport, moisture enters this area mainly from south boundary. For the zonal moisture transport, moisture enters through west boundary and departs from east boundary all the year. Overall, the period of positive moisture budget is from February to October calculated by moisture transport method, and from February to September by the other two methods. Vertical distribution of moisture budget is calculated by moisture transport method and moisture flux divergence method. It shows that the anomaly transport between 800—500 hPa is positive during 1960s and early 1970s and negative after that. Below 800 hPa, the values manifest negative before 1960s, and then turn to positive. There is net income of moisture at the whole layer except for the 850 hPa. By moisture flux divergence method, the calculated moisture convergence is positive above 450 hPa, and negative below. The interannual moisture budget variability of four seasons is quite obvious.
    • FullText(HTML)
    References(31)

  • Fig. 1  Humid region affected by East Asian Monsoon

    DownLoad: Full-Size Img PowerPoint

    Fig. 2  Climatic distribution of the annual average moisture transport in humid region affected by East Asian Monsoon from 1958 to 2007(unit: kg • s-1 • m-1, the value of moisture transport flux in shadow area exceeds 100 kg • s-1 • m-1)

    DownLoad: Full-Size Img PowerPoint

    Fig. 3  The climatological average zonal and meridional cycle of moisture budget in humid region affected by East Asian Monsoon from 1958 to 2007

    (a) from the west boundary, (b) from the east boundary, (c) the zonal net budget anomaly, (d) from the south boundary, (e) from the north boundary, (f) the meridional net budget anomal

    DownLoad: Full-Size Img PowerPoint

    Fig. 4  The climatological cycle of the moisture budget anomaly calculated by the moisture transport, moisture llux divergence and P-E motheds in humid region affected by East Asian Monsoon averaged from 1958 to 2007

    DownLoad: Full-Size Img PowerPoint

    Fig. 5  The time-zone distribution and time-meridian distribution of moisture transport under the climatic mean state in humid region affected by East Asian

    Monsoon from 1958 to 2007 (the value of shadow area exceeds 100kg·s-1·m-1) (a) B boundary, (b) D boundary, (c) F boundary, (d) A boundary, (e) C boundary, (f) E boundary

    DownLoad: Full-Size Img PowerPoint

    Fig. 6  The interannual change of the vertical distribution of moisture budget anomaly calculated by moisture transport method in humid region affected by East Asian Monsoon from 1958 to 2007(unit:104 m3·s-1) (the value of heavy shadow area exceeds1×104 m3·s-1, the light shadow area is below-1×104 m3·s-1)

    DownLoad: Full-Size Img PowerPoint

    Fig. 7  The vertical distribution of climatological mean moisture budgetcalculated by moisture transport method under the climatic mean state inhumid region affected by East Asian Monsoon from 1958 to 2007

    DownLoad: Full-Size Img PowerPoint

    Fig. 8  The interannual changes of moisture budget anomaly calculated by the moisture transport, moisture flux divergence and P~E methods in humid region affected by East Asian Monsoon from 1958 to 2007 (a) annual budget, (b) spring, (c) summer, (d) autumn, (d) winter

    DownLoad: Full-Size Img PowerPoint

    Table  1  The seasonal variability of moisture budget calculated by moisture transport in humid region affected by East Asian Monsoon from 1958

    Table  2  The seasonal variability and absolute error of themoisture budget calculated by and in humid region affected by East Asian Monsoonfrom 1958 to 2007 (unit:104 m3 • s-1)
  • [1]
    高由禧, 徐淑英.关于东亚季风区域的气候的研究.气象学报, 1959, 30(3):258-262. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB195903011.htm
    [2]
    HoL, Wang B.The time space structure of the Asian-Pacific summer monsoon:A fast annual cycle view.J Climate, 2002, 15(15):2001-2019. doi:  10.1175/1520-0442(2002)015<2001:TTSSOT>2.0.CO;2
    [3]
    孙林海, 赵振国, 许力, 等.中国东部季风区夏季雨型的划分及其环流成因分析.应用气象学报, 2005, 16(3):56-62. http://www.cnki.com.cn/Article/CJFDTOTAL-YYQX2005S1006.htm
    [4]
    赵平, 周秀骥.近40年我国东部降水持续时间和雨带移动的年代际变化.应用气象学报, 2006, 17(5):548-556. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20060594&flag=1
    [5]
    陈隆勋.东亚季风.北京:气象出版社, 1991.
    [6]
    王劲松, 陈发虎, 靳立亚, 等.亚洲中部干旱区在20世纪两次暖期的表现.冰川冻土, 2008, 30(2):224-233. http://www.cnki.com.cn/Article/CJFDTOTAL-BCDT200802007.htm
    [7]
    Rasmusson E M.Atmospheric water vapor transport and the water balance of North America.Part I:Characteristics of the water vapor flux field.Mon Wea Rev, 1967, 95:403-426. doi:  10.1175/1520-0493(1967)095<0403:AWVTAT>2.3.CO;2
    [8]
    Rasmusson E M, Mo K C.Large-scale atmospheric moisture cycling as evaluated from NMC global analysis and forecast products.J Climate, 1996, 9:3276-3297. doi:  10.1175/1520-0442(1996)009<3276:LSAMCA>2.0.CO;2
    [9]
    Roads JO, Chen S C, Guetter A K, et al.Large-scale aspects of the United States hydrological cycle.Bull Amer Meteor Soc, 1994, 75:1589-1610. doi:  10.1175/1520-0477(1994)075<1589:LSAOTU>2.0.CO;2
    [10]
    Schmitz J T, Mullen S L.Water vapor transport associated with summertime North American monsoon as depicted by ECWMF analyses.J Climate, 1996, 9:1621-1634. doi:  10.1175/1520-0442(1996)009<1621:WVTAWT>2.0.CO;2
    [11]
    Trenberth K E, Guillemot C J.Evaluation of the atmospheric moisture and hydrological cycle in the NCEP/NCAR reanalyses.Climate Dynamics, 1998, 14:213-231. doi:  10.1007/s003820050219
    [12]
    Bisslink B, Dolman A J.Precipitation recycling:Moisture sources over Europe using ERA-40 data.Journal of H ydrometeorology, 2008, 9(10):1073-1083.
    [13]
    Serreze M C, Roger G.Atmospheric water vapor characteris-tics at 70°N.J Climate, 1995, 8(4):719-731. doi:  10.1175/1520-0442(1995)008<0719:AWVCA>2.0.CO;2
    [14]
    Zangvil A, Portis D H, Lamb P J.Investigation of the large-scale atmospheric moisture field over the Midwestern United States in relation to summer precipitation.Part I:Relation-ships between moisture budget components on different time scales.J Climate, 2000, 14:582-597.
    [15]
    Simmonds I, Bi D H, Hope P.Atmospheric water vapor flux and it sassociation with rainfall over China in summer.J Climate, 1999, 12(5):1353-1367. doi:  10.1175/1520-0442(1999)012<1353:AWVFAI>2.0.CO;2
    [16]
    Ninimiya K.Moisture balance over China and the South China Sea during the summer monsoon in relation to the intense rainfalls over China.J Meteor Soc Japan, 1999, 77(3): 737-751.
    [17]
    Knippert z P, Wernli H.A Lagrangian climatology of tropical moisture exports to the Northern Hemispheric extratropics. J Climate, 2010, 23(2):987-1003. http://www.academia.edu/13574968/A_Lagrangian_Climatology_of_Tropical_Moisture_Exports_to_the_Northern_Hemispheric_Extratropics
    [18]
    周天军, 张学洪, 王绍武.全球水循环的海洋分量研究.气象学报, 1999, 57(3):264-282. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB903.001.htm
    [19]
    黄荣辉, 张振洲, 黄刚, 等.夏季东亚季风区水汽输送特征及其与南亚季风区水气输送的差别.大气科学, 1998, 22 (4):460-469. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK804.007.htm
    [20]
    范广洲, 吕世华, 程国栋.华北地区夏季水量丰、枯年大气水分收支对比分析.兰州大学学报 (自然科学版), 2001, 37 (3):134-141.
    [21]
    苗秋菊, 徐祥德, 张胜军.长江流域水汽收支与高原水汽输送分量"转换"特征.气象学报, 2005, 63(1):93-99.
    [22]
    赵瑞霞, 吴国雄, 张宏.夏季风期间长江流域的水汽输送状态及其年际变化.地球物理学报, 2008, 51(6):1670-1681. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX200806008.htm
    [23]
    赵瑞霞, 吴国雄.黄河流域中上游水分收支以及再分析资料可用性分析.自然科学进展, 2006, 16(3):316-324. http://www.cnki.com.cn/Article/CJFDTOTAL-ZKJZ200603012.htm
    [24]
    赵瑞霞, 吴国雄.长江流域水分收支以及再分析资料可用性分析.气象学报, 2007, 65(3):416-427. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB200703009.htm
    [25]
    张文君, 周天军, 宇如聪.中国东部水分收支的初步分析.大气科学, 2007, 31(2):329-345. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200702014.htm
    [26]
    张洁, 周天军, 宇如聪, 等.中国春季典型降水异常及相联系的大气水汽输送.大气科学, 2009, 33(1):121-134. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200901010.htm
    [27]
    谢安, 毛江玉, 宋焱云, 等.长江中下游地区水汽输送的气候特征.应用气象学报, 2002, 13(1):67-77. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20020108&flag=1
    [28]
    施小英, 施晓晖.夏季青藏高原东南部水汽收支气候特征及其影响.应用气象学报, 2008, 19(1):41-46. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20080108&flag=1
    [29]
    Yanai M, Esbensen S, ChuJ H.Determination of average bulk properties of tropical cloud clusters from largerscale heat and moisture budgets.Journal of Atmospheric Science, 1973, 30 (4):611-627. doi:  10.1175/1520-0469(1973)030<0611:DOBPOT>2.0.CO;2
    [30]
    Rasmusson E M.Atmospheric water vapor transport and the water balance of North America.Part II:Large-scale water balance investigations.Mon Wea Rev, 1968, 96:720-724. doi:  10.1175/1520-0493(1968)096<0720:AWVTAT>2.0.CO;2
    [31]
    Barry R G.Variations in the content and flux of water vapor over north-eastern North America during two winter seasons. Quarterly Journal of the Royal Meteorological Society, 1967, 93:535-543. doi:  10.1002/(ISSN)1477-870X
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中
  • -->

Catalog

    Figures(8)  / Tables(2)

    Get Citation
    PDF
    XML
    Article views (4539) PDF downloads(1914) Cited by()
    • Received : 2010-03-29
    • Accepted : 2010-10-08
    • Published : 2010-12-31
    Journal Online
    Contact

    © 2020 Journal of Applied Meteorological Science   京ICP备15006967号-1

    Supported by Beijing Renhe Information Technology Co. Ltd

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return