CHEN Yu-hang,FAN Guang-zhou,ZHANG Yong-li,et al.The Analysis of Underlying Variation Characteristics over Tibetan Plateau based on GLDAS Data[J].Journal of Chengdu University of Information Technology,2016,(02):204-212.
基于GLDAS资料的青藏高原下垫面变化特征分析
- Title:
- The Analysis of Underlying Variation Characteristics over Tibetan Plateau based on GLDAS Data
- 文章编号:
- 2096-1618(2016)02-0204-09
- Keywords:
- atmospheric science; climate change; Tibetan Plateau; underlying; GLDAS
- 分类号:
- P463.1
- 文献标志码:
- A
- 摘要:
- 为了研究青藏高原下垫面气候变化特征,利用全球陆面数据同化系统逐月资料,采用线性回归和滑动T检验等方法,对青藏高原下垫面物理量的年际变化、年际变化空间分布进行初步分析,同时分季节讨论各物理量的年际变化特征。结果表明:1948~2010年高原下垫面逐渐趋于暖湿化,能量与水分循环发生着显著的变化,高原下垫面能量变化快于水分循环变化。各要素年际变化在各个季节表现出不同的特征。高原气候变化总体表现为:地表净短波辐射减弱,净长波辐射增强。随着净短波辐射的减弱,感热通量表现出相同的变化趋势。随着总蒸散的增强,潜热通量增加。下垫面温度升高,降水增多。植被冠层含水量、地表径流增加。地温升高,使得下垫面土壤湿度加大。地表气压增加,风速减弱,比湿降低。各要素年际变化存在明显的区域特征。
- Abstract:
- Using the monthly data of Global Land Data Assimilation System and the method of linear regression and the sliding t-test, the inter-annual variability of underlying physical variables over the Tibetan Plateau(TP)and the change's spatial distribution are initially investigated and the inter-annual variability also discussed by season in order to study the feature of underlying change over TP. The results are as follows: The underlying surface of the TP tended to warm and humid from 1948 to 2010. Energy and water cycle undergo significant change. Energy cycle trend to change faster than the hydrological cycle. The climate change of elements in all seasons exhibit different characteristics. The overall performance of the TP climate change: net shortwave radiation weakens and net long wave radiation increases. With the weakening of net short-wave radiation, sensible heat flux show the same trends. With the enhancement of total evapotranspiration, latent heat flux increases. Underlying temperature is rising and precipitation become more. Both vegetation canopy water content and surface runoff slowly increase. Soil temperature's rising make the underlying surface soil moisture increase. Surface pressure get enhanced. Wind speed tends to. Near surface specific humidity decreases. Each element has a significant regional variation.
参考文献/References:
[1] 陈泮勤.世界气候研究计划(WCRP)及其进展[J].1995,地球科学进展,10(5):488-491.
[2] 孙成权,张志强,国际全球变化研究计划综览[J].地球科学进展, 1994,9(3),53-70.
[3] 潘保田,李吉均.青藏高原:全球气候变化的驱动机与放大器.Ⅲ.青藏高原隆起对气候变化的影响[J].兰州大学学报,1996,32(1):108-115.
[4] 姚檀栋,朱立平.青藏高原环境变化对全球变化的响应及其适应对策[J].地球科学进展,2006,21(5):459-464.
[5] 卢爱刚,何元庆,张忠林,等.中国大陆对全球变暖响应的区域敏感性分析[J].冰川冻土,2005,27(6):827-832.
[6] 林振耀,赵听奕.青藏高原气温降水变化的空间分布[J].中国科学(D辑),1996,26(4):354-358.
[7] 吴绍洪,尹云鹤,郑度,等.青藏高原近30年气候变化趋势[J].地理学报,2005,60(1):3-11.
[8] 牛涛,刘洪利,宋燕,等.青藏高原气候由暖干到暖湿时期的年代际变化特征研究[J].应用气象学报,2005,16(6):763-771.
[9] 李林,朱西德,王振宇,等.青藏高原气候变化趋于暖湿化的若干事实[C].第26届中国气象学会年会气候变化分会场论文集,2009:936-942.
[10] Oku Y, Ishikawa H, Su Z. Estimation of Land Surface Heat Fluxes over the Tibetan Plateau Using GMS Data[J]. Journal of Applied Meteorology and Climatology, 2007, 46(2):183-195.
[11] Duan A, Wu G. Change of cloud amount and the climate warming on the Tibetan Plateau [J]. Geophysical Research Letters, 2006, 33(22):217-234.
[12] 程志刚,刘晓东,范广洲,等. 21世纪青藏高原气候时空变化评估[J].干旱区研究,2011,28(4):669-676.
[13] Yang K,Wu H,Qin J,et al.Recent climate changes over the Tibetan Plateau and their impacts on energy and water cycle:A review [J].Globals&splanetary Change,2014,112(1):79-91.
[14] Vautard R, Cattiaux J, Yiou P, et al. Northern Hemisphere atmospheric stilling partly attributed to an increase in surface roughness [J]. Nature Geoscience, 2010, 3(11):756-761.
[15] You Q, Kang S, Flugel W, et al. Decreasing wind speed and weakening latitudinal surface pressure gradients in the Tibetan Plateau [J]. Climate Research, 2010, 42(1):57-64.
[16] Lin C, Yang K, Qin J, et al. Observed Coherent Trends of Surface and Upper-Air Wind Speed over China since 1960[J]. Journal of Climate, 2013, 26(9):2891-2903.
[17] Yang K, Ye B, Zhou D, et al. Response of Hydrological Cycle to Recent Climate Changes in the Tibetan Plateau [J]. Climatic Change, 2011, 109(3-4):517-534.
[18] You Q, Sanchez-Lorenzo A, Wild M, et al. Decadal variation of surface solar radiation in the Tibetan Plateau from observations, reanalysis and model simulations[J]. Climate Dynamics, 2013, 40(7-8):2073-2086.
[19] You Q, Kang S, Flügel W, et al. From brightening to dimming in sunshine duration over the eastern and central Tibetan Plateau(1961-2005)[J]. Theoretical and Applied Climatology, 2010, 101(3-4):445-457.
[20] Yang K, Ding B, Qin J, et al. Can aerosol loading explain the solar dimming over the Tibetan Plateau? [J]. Geophysical Research Letters, 2012, 39(20).
[21] Li Z, Wei Z, Lü S, et al. Effect of land surface processes on the Tibetan Plateau's past and its predicted response to global warming: an analytical investigation based on simulation results from the CMIP5 model [J]. Environmental Earth Sciences, 2014, 72(4):1155-1166.
[22] Xu X, Lu C, Shi X, et al. World water tower: An atmospheric perspective [J]. Geophysical Research Letters, 2008, 35(20):525-530.
[23] Qinglong You, Shichang Kang, Yanhong Wu, et al. Climate change over the Yarlung Zangbo River Basin during 1961-2005[J]. Journal of Geographical Sciences, 2007, 17(4):409-420.
[24] Zhang Y, Liu C, Tang Y, et al. Trends in pan evaporation and reference and actual evapotranspiration across the Tibetan Plateau [J]. Journal of Geophysical Research Atmospheres, 2007, 112(D12):1103-1118.
[25] Li X, Jin R, Pan X, et al. Changes in the near-surface soil freeze–thaw cycle on the Qinghai-Tibetan Plateau [J]. International Journal of Applied Earth Observation and Geoinformation, 2012, 17(7):33–42.
[26] Ren L, Lin Z, Yong-jian D, et al. The Climatic Characteristics of the Maximum Seasonal Frozen Depth in the Tibetan Plateau [J]. Journal of Glaciology and Geocryology, 2009, 31(6):1050-1056.
[27] Wu Q, Zhang T. Changes in active layer thickness over the Qinghai‐Tibetan Plateau from 1995 to 2007[J]. Journal of Geophysical Research Atmospheres, 2010, 115(D9):736-744.
[28] IPCC, 2014: Climate Change 2014: Synthesis Report. Contribution of Working Groups I, II and III to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Core Writing Team, R.K. Pachauri and L.A. Meyer(eds.)]. IPCC, Geneva, Switzerland, 151 pp.
[29] 吴国雄,刘屹岷,刘新,等.青藏高原加热如何影响亚洲季风的气候格局[J].大气科学, 2005,29(1):47-56.
[30] 王婉昭,高艳红,许建伟.青藏高原及其周边干旱区气候变化特征与GLDAS适用性分析[J].高原气象, 2013,32(3):635-645.
[31] Wang A, Zeng X. Evaluation of multireanalysis products with in situ observations over the Tibetan Plateau [J]. Journal of Geophysical Research Atmospheres, 2012, 117(D5):214-221.
[32] 王文,汪小菊,王鹏. GLDAS月降水数据在中国区的适用性评估[J].水科学进展,2014,25(6):769-778.
[33] M W, H G, A R, et al. From dimming to brightening: Decadal changes in solar radiation at Earth's surface [J]. Science, 2005, 308: 847–850.
[34] Moore G W K. Surface pressure record of Tibetan Plateau warming since the 1870s [J]. Quarterly Journal of the Royal Meteorological Society, 2012, 138(669):1999–2008.
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备注/Memo
收稿日期:2015-04-23 基金项目:国家自然科学基金资助项目(41275079、41405069); 国家青年科学基金资助项目(41305077)