Regional differences in the surface energy budget over China: an evaluation of a selection of CMIP5 models

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• 作者：Lian-Tong Zhou ; Zhencai Du
• 刊名：Theoretical and Applied Climatology
• 出版年：2016
• 出版时间：April 2016
• 年：2016
• 卷：124
• 期：1-2
• 页码：241-266
• 全文大小：6,505 KB
• 参考文献：Beljaars ACM (1997) Air-sea interaction in the ECMWF model. Proc. Seminar on Atmosphere-Surface Interaction. Reading, United Kingdom, ECMWF, 33–52
  Bueh CL, Ji LR, Cui MC (2002) Energy balance of land surface process in the arid and semi-arid regions of China and its relation to the regional atmospheric circulation in summer. Clim Environ Res 7(1):61–73
  Curry JA, Ebert EE (1992) Annual cycle of radiation fluxes over the Arctic ocean: sensitivity to cloud properties. J Clim 5:1267–1280CrossRef
  Curry JA, Ebert EE, Schramm JL (1993) Impact of clouds on the surface radiation balance of the Arctic Ocean. Meteorol Atmos Phys 51:197–217CrossRef
  Curry JA, Rossow WB, Randall D, Schramm JL (1996) Overview of Arctic cloud and radiation characteristics. J Clim 9:1731–1763CrossRef
  Fairall CW, Bradley EF, Rogers DP, Edson JB, Young GS (1996) Bulk parameterization of air-sea fluxes for TOGA COARE. J Geophys Res 101:3747–3764CrossRef
  Gao R, Dong WJ, Wei ZG (2008) Numerical simulation of the impact of abnormity of sensible heat flux in northwest arid zone on precipitation in China. Plateau Meteorol 27(2):320–324
  Gibson JK, Kallberg P, Uppala S, Hernandez A, Normura A, Serrano E (1997) ERA description, ECMWF reanalysis project report series1, ECMWF. Reading, 66pp
  Hui XY, Wang CH, Zuo HC, Dong WJ (2005) Abnormal features of sensible and latent heat fluxes in arid region of Northern China. Plateau Meteorol 24(3):415–421
  Josey SA (2001) A comparison of ECWMF, NCEP-NCAR, and SOC surface heat fluxes with moored buoy measurements in the subduction region of the northeast Atlantic. J Clim 14:1780–1789CrossRef
  Kalnay E, Kanamitsu M, Kistler R et al (1996) The NCEP-NCAR 40-year reanalysis project. Bull Am Meteorol Soc 77:437–471CrossRef
  Kistler R, Kalnay E, Collins W et al (2001) The NCEP-NCAR 50-year reanalysis: monthly means CD-ROM and documentation. Bull Am Meteorol Soc 82:247–262CrossRef
  Kubota M, Kano A, Muramatsu H, Tomita H (2003) Intercomparison of various surface latent heat flux fields. J Clim 16:670–678CrossRef
  Liu J, Curry JA, Rossow WB, Key JR, Wang X (2005) Comparison of surface radiative flux data sets over the Arctic Ocean. J Geophys Res 110(C02015). doi:10.​1029/​2004JC002381
  Qu Y, Gao X, Chen W et al (2008) Comparison of surface air temperatures and precipitation in Eastern and Western China during 1951–2003. Plateau Meteorol 27(3):524–529, in Chinese
  Renfrew IA, Moore GWK, Guest PS, Bumke K (2002) A comparison of surface layer and surface turbulent flux observations over the Labrador Sea with ECMWF reanalyses and NCEP reanalyses. J Phys Oceanogr 32:383–400CrossRef
  Serreze MC et al (2000) Observational evidence for recent changes in the northern high-latitude environment. Clim Chang 46:159–207CrossRef
  Siefridt L, Barnier B, Beranger K, Roquet H (1999) Evaluation of operational ECMWF surface heat fluxes: impact of parameterization changes during 1986–1996. J Mar Syst 19:113–135CrossRef
  Smith SR, Legler DM, Verzone KV (2001) Quantifying uncertainties in NCEP reanalyses using high-quality research vessel observations. J Clim 14:4062–4072CrossRef
  Sorteberg A, Kattsov V, Walsh JE, Pavlova T (2007) The Arctic surface energy budget as simulated with the IPCC AR4 AOGCMs. Clim Dyn 29:131–156. doi:10.​1007/​s00382-006-0222-9 CrossRef
  Sun B, Yu L, Weller RA (2003) Comparison of surface meteorology and turbulent heat fluxes over the Atlantic: NWP model analyses versus moored buoy observations. J Clim 16:679–695CrossRef
  Taylor KE, Stouffer RJ, Meehl GA (2012) An overview of CMIP5 and the experiment design. Bull Amer Meteor Soc 93:485–498. doi:10.​1175/​BAMS-D-11-00094.​1
  Uppala S (2002) ECMWF reanalysis,1957-2001, ERA-40. ERA-40 Project Report Series, 3:1–10
  Weller RA, Anderson SP (1996) Surface meteorology and air-seafluxes in the western equatorial Pacific warm pool during the TOGA COARE. J Clim 9:1959–1990CrossRef
  White GH (1995) An intercomparison of precipitation and surface fluxes from operational NWP analysis/forecast systems. WMOCAS/JSC Working Group on Numerical Experimentation Rep. 22:WMO/TD-723,33p
  Zeng X, Zhao M, Dickinson RE (1998) Intercomparison of bulk aerodynamic algorithms for the computation of sea surface fluxes using the TOGA COARRE and TAO data. J Clim 11:2628–2644CrossRef
  Zhang J, Wu L (2014) Impacts of land-atmosphere interactions on climate over East Asia. China Meteorological Press, Beijing, pp 91–108
  Zhang T, Bowling SA, Stamnes K (1997) Impact of the atmosphere on surface radiative fluxes and snowmelt in the Arctic and Subarctic. J Geophys Res 102(D4):4287–4430CrossRef
  Zhang Q, Wei GA, Huang RH (2001) Momentum and bulk sensible heat transfer coefficient over Gobi in Northwest China. Sci China (Ser D) 31:783–792
  Zhang Q, Wei GA, Huang RH (2003) The field experiment on local surface process of Dunhuang in arid region. In: Guoxiong W et al (eds) Collected papers of the project “Research on the Formation Mechanism and Prediction Theory of Severe Climatic Disasters in China” III, influence of Tibet and arid region on climatic disasters (in Chinese). China Meteorological Press, Beijing, pp 157–177
  Zhang Q, Huang RH, Wang S, Wei GA, Cao XY, Hou XH, Lu SH, Hu ZY, Ma YM, Wei ZG, Nie JN, Gao HC, Gao HM, Yan YP (2005) NWC-ALIEX and its research advances. Adv Earth Sci 20:427–441
  Zhou LT (2009) Difference in the interdecadal variability of spring and summer sensible heat fluxes over Northwest China. Atmos Ocean Sci Lett 2:119–123CrossRef
  Zhou LT (2011) Interdecadal variability in surface solar radiation over Northwest China and its possible cause. Atmos Ocean Sci Lett 4(2):103–108CrossRef
  Zhou LT, Huang RH (2008) Interdecadal variability of sensible heat flux in arid and semi-arid region of Northwest China and its relationship to summer precipitation in China. Chin J Atmos Sci 32:1276–1288, in Chinese
  Zhou LT, Huang RH (2010a) Interdecadal variability of summer rainfall in Northwest China and its possible causes. Int J Climatol 30:549–557. doi:10.​1002/​joc.​1923
  Zhou LT, Huang RH (2010b) An assessment on the quality of surface sensible heat flux derived from re-analysis data based on station observations in Northwest China. Adv Atmos Sci 27(3):530–544. doi:10.​1007/​s00376-009-9081-8
  Zhou LT, Huang RH (2014) Regional differences in surface sensible and latent heat fluxes in China. Theor Appl Climatol 116:625–637. doi:10.​1007/​s00704-013-0975-0 CrossRef
  Zhou LT, Wu R, Huang RH (2010) Variability of surface sensible heat flux over Northwest China. Atmos Ocean Sci Lett 3(2):75–80CrossRef
  
• 作者单位：Lian-Tong Zhou (1)
  Zhencai Du (1) (2) (3)
  
  1. Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences, P.O. Box 2718, Beijing, 100190, China
  2. State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State Oceanic Administration, Hangzhou, China
  3. P.O. Box 5111, Beijing, China
  
• 刊物类别：Earth and Environmental Science
• 刊物主题：Earth sciences
  Meteorology and Climatology
  Atmospheric Protection, Air Quality Control and Air Pollution
  Climate Change
  Waste Water Technology, Water Pollution Control, Water Management and Aquatic Pollution
  
• 出版者：Springer Wien
• ISSN：1434-4483

文摘

The present study provides an evaluation of the regional differences over China in surface energy budget components as simulated by a selection of models from phase five of the Coupled Model Intercomparison Project (CMIP5), covering the period 1960–2005. Similarities and differences exist among the models in terms of both spatial and magnitude patterns. For climatology, the CMIP5 models show quite different spatial distributions of shortwave radiation and sensible heat flux. In terms of seasonal variation, the surface energy budgets are remarkably different between western and eastern China. The discrepancies in the seasonal variation of sensible heat flux are mainly attributable to temperature differences and wind speed, while those of shortwave radiation are caused by the seasonal variation in total cloud cover. Cloudiness is one of the most crucial parameters in estimating the surface energy budget. In addition, the study also reveals that the magnitudes of the various components show larger (more than two-fold) differences between western and eastern parts of China, especially in net longwave and upward shortwave radiation, as well as latent and sensible heat fluxes. The results for surface soil heat flux show that there is more incoming energy during spring and summer and more outgoing energy during fall and winter in both western and eastern China. Furthermore, compared to NCEP2 data, the ERA-40 reanalysis product produces results more similar to the multi-model ensemble mean for most components.