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IGARSS 2011, Jul. 26, Vancouver 1 Improving Land Surface Energy and Water Fluxes Simulation over the Tibetan Plateau with Using a Land Data Assimilation.

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Presentation on theme: "IGARSS 2011, Jul. 26, Vancouver 1 Improving Land Surface Energy and Water Fluxes Simulation over the Tibetan Plateau with Using a Land Data Assimilation."— Presentation transcript:

1 IGARSS 2011, Jul. 26, Vancouver 1 Improving Land Surface Energy and Water Fluxes Simulation over the Tibetan Plateau with Using a Land Data Assimilation System Hui Lu (Tsinghua University) Toshio Koike, Hiroyuki Tsutsui, Katsunori Tamagawa (The University of Tokyo) Kun Yang, Xin Li (Chinese Academy of Science) Xiangde Xu (Chinese Meteorological Admistration)

2 IGARSS 2011, Jul. 26, Vancouver 2 Contents Background and Objective Land Data Assimilation System Application Region and Data –Simulation domain and ground sites –Used Data Results –Surface soil moisture –Land surface energy fluxes Remarks

3 IGARSS 2011, Jul. 26, Vancouver 3 Background and objective Tibetan Plateau is important in the progress of the Asian summer monsoon –land surface processes –direct Orographic and thermal effects Land-atmosphere interaction in T-P is the key to –improve the understanding of Asian monsoon –improve the accuracy of numerical weather prediction in east Asia –mitigate weather disaster in this region Objectives of this research –To identify the potential of LDAS to improve the modeling of land surface fluxes. –To generate reliable regional distribution of soil moisture and energy fluxes

4 IGARSS 2011, Jul. 26, Vancouver 4 Land Data Assimilation System Why LDAS –Shortage of model Maybe biased, can not correct errors from forcing, parameter setting and model physics –Shortage of satellite remote sensing Limited information, both temporal and spatial Structure of LDAS: three parts of a variational system –Dynamic model: Land surface scheme : SiB2 –TB observation: RTM: Advanced Integral Equation Method (AIEM) –Optimization scheme: Shuffled Complex Evolution (SCE)

5 IGARSS 2011, Jul. 26, Vancouver 5 LSM Minimization scheme F(Tb obs -Tb sim ) Tg, Tc, Mv Tb sim Mv Vegetation layer Surface Surface radiationVegetation emission RTM Tb obs Microwave TMI/AMSR/AMSR-E (6.9/10.6 and 18.7 GHz) SiB2/New SiB DMRT-AIEM Shuffled Complex Evolution Optimization + Assimilation LDAS

6 IGARSS 2011, Jul. 26, Vancouver 6 Introduction of LDAS-UT: Input and Output LDAS-UT Meteorological Forcing Meteorological Forcing: Wind, Temp., Humidity, Pressure, Precipitation, Radiation In situ observation, Satellite Products, model outputs, Default Parameters: Land Cover Type, Soil Type, …… ISLSCP Output Status Variables Output Status Variables: Energy fluxes Soil Moisture profile Soil Temp. profile Canopy Temperature …… Semi-dynamic Vegetation information Semi-dynamic Vegetation information: MODIS, LAI  VWC MODIS, NDVI  Vegetation Fractional coverage: Observation: Microwave TB TMI/AMSR/AMSR-E

7 IGARSS 2011, Jul. 26, Vancouver 7 Application Region Domain: –Lat: 25-40N –Lon: 70-105E Simulated Period –May. - Sep., 2008 Two local sites –West: Gaize –East: Naqu

8 IGARSS 2011, Jul. 26, Vancouver 8 Used Data In situ observation –Soil moisture at two sites –AWS observation –Energy fluxes derived from AWS observation by Bowen Ratio Reanalysis data from NCEP –Meteorological forcing for region simulation –Biases in radiation and precipitation, but not corrected for regional application. Satellite remote sensing data –Soil moisture retrieval from AMSR-E (JAXA) –Brightness temperature from AMSR-E

9 IGARSS 2011, Jul. 26, Vancouver 9 Results Soil Moisture

10 IGARSS 2011, Jul. 26, Vancouver 10 Result: Soil moisture at Gaize MBERMSER LDAS2.748.460.361 AMSR-E-3.016.130.601 NCEP25.2826.130.442

11 IGARSS 2011, Jul. 26, Vancouver 11 Result: Soil moisture at Naqu MBERMSER LDAS-0.173.880.853 AMSR-E10.1621.250.562 NCEP10.0212.150.417

12 IGARSS 2011, Jul. 26, Vancouver 12 Result: Energy flux:Bowen Ratio Clean wet/dry division is showed by LDAS result, while NCEP failed to represent such a feature.

13 IGARSS 2011, Jul. 26, Vancouver 13 Result: energy fluxes at Gaize MBERMSER Hs43.3854.210.879 lE12.8831.050.878 G0-15.0977.190.949

14 IGARSS 2011, Jul. 26, Vancouver 14 Result: energy fluxes at Naqu MBERMSER Hs35.6442.360.934 lE6.9335.140.975 G03.7268.850.967

15 IGARSS 2011, Jul. 26, Vancouver 15 Result: Dynamic variation Cyclonic brings moisture from the Bay of Bengal to the SE of T-P, and brings dry air mass from Taklamagan desert LDAS-UT is able to provide more realistic land surface status for research in other principles LDAS-UT NCEP

16 IGARSS 2011, Jul. 26, Vancouver 16 Remark Land-atmosphere interaction in T-P is very important for Asian monsoon development. Combining MW remote sensing and LSM, LDAS could improve the land surface fluxes simulation. LDAS produce more realistic land surface status, which is in good agreement with monsoon development. Feeding LDAS fluxes into atmosphere model is expected

17 IGARSS 2011, Jul. 26, Vancouver 17 Acknowledgments The data is get from “ Japan-China JICA project ”. Colleges contribute to this project are: –UT: T. Koike, K. Tamagawa, H. Tutsui, L. Wang –Tsukuba U.: K. Ueno –ITP: K. Yang, Y.M. Mao –CAREERI: X. Li, Z.Y. Hu, W.Q. Ma, M.S.Li –CAMS: X.D. Xu, H. Peng

18 IGARSS 2011, Jul. 26, Vancouver 18 Thank you for your attention!


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