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1 Yun Fan, Huug van den Dool, Dag Lohmann, Ken Mitchell CPC/EMC/NCEP/NWS/NOAA Kunming, May, 2004.

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Presentation on theme: "1 Yun Fan, Huug van den Dool, Dag Lohmann, Ken Mitchell CPC/EMC/NCEP/NWS/NOAA Kunming, May, 2004."— Presentation transcript:

1 1 Yun Fan, Huug van den Dool, Dag Lohmann, Ken Mitchell CPC/EMC/NCEP/NWS/NOAA Kunming, May, 2004

2 2 Motivations Improve soil moisture data for CPC’s drought & flood monitoring tools Improve land surface model via data validation and model intercomparisons Provide model consistent initial conditions for various ranging forecasts Provide a long time series of realistic land surface data for land memory & predictablity studies Coupled atmosphere-land-ocean modeling Other……

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4 4 CPC Leaky Bucket Soil Moisture Model (Huang et al 1996) The soil moisture budget over an area A: Where W(t) is soil water content P(t) precipitation E(t) evaportranspiration R(t) net streamflow divergence G(t) net groundwater loss Forcing Data: -CPC daily temperature updates -CPC daily precipitation updates (Higgins & Shi) -Monthly precipitation and temperature from NCDC

5 5 CPC Leaky Bucket Soil Moisture Model - cont Output Data Coverage: - 72 years (1931-yesterday) on 344 US climate divisions - 56+ years (1948-present) on global domain Products Web Site (daily & monthly updated): - http://www.cpc.ncep.noaa.gov/soilmst / (official site) - http://www.cpc.ncep.noaa.gov/soilmst/index.htm (test site)

6 Current CPC soil moisture related monitoring & predictive activities: – Drought & flood monitoring – Empirical forecast tools (Constructed Analog) – GFS forecast & climate prediction

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8 CPC Leaky Bucket Model - Monitoring

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11 CPC Leaky Bucket Model - GFS bias corrected ensemble forecasts (daily Prcp and Temp at 0Z) are used to drive the soil moisture model.

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14 CPC Leaky Bucket Model CA Monthly and Seasonal Forecasts

15 15 Retrospective LDAS Run Project A joint project to Land Data Assimilation System (LDAS) Project NOAH Land Surface Model –Physically far more complete –Higher resolution (spatial: 1/8 degree grid, temporal: hourly) Forcing Data (1948-1998): –Observed precip (Higgins & Shi) –Atmospheric forcing (From global reanalysis) Outputs Will Provide: –Improved soil moisture & associated land data variables. –Superior model consistent initial conditions –others

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20 Data validation cr=0.70 cr=0.73 cr=0.55

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26 Jan &Jul Climatology (1961-1990) of all water balance components

27 Land Surface Water Budget Over Conterminous USA

28 Mon W P E R+G P-E-R-G 1 581.2 (294.2) 52.0 5.5 31.8 14.6 2 592.5 (304.0) 49.8 10.3 33.3 6.2 3 600.0 (308.8) 62.9 24.5 39.1 -0.7 4 595.6 (302.0) 59.4 42.8 30.2 -13.7 5 582.8 (289.8) 70.9 64.8 21.2 -15.1 6 564.6 (276.8) 66.2 75.7 14.2 -23.8 7 538.4 (260.1) 64.8 77.8 10.4 -23.5 8 520.1 (250.0) 62.2 67.6 9.0 -14.3 9 514.3 (248.3) 61.4 49.3 8.8 3.3 10 520.2 (253.3) 51.7 31.9 9.1 10.8 11 539.8 (266.8) 58.0 14.0 13.5 30.5 12 565.8 (282.6) 58.5 4.5 27.3 26.8 Year 559.0 (278.1) 59.8 39.1 20.7 0.0 averaged over 125W-75W, 30N-48N US monthly values of all components of land surface hydrology (mm/mon)

29 P(t) - E(t) - R(t) – G(t)

30 Simulated extreme hydrologic events: 1988 drought & 1993 flood

31 31 Summary & Future Work Summary & Future Work Monitoring & predicting land surface variables LSMs can simulate some realistic land features Need more detailed analysis & studies –Data validation, model comparisons & improvements –Modeling & Prediction experiments Global Retrospective LDAS Run Others


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