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Bob Joyce : RSIS, Inc.

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Global, Microwave-based, Precipitation Analyses from Satellite at Hr & 8 km Scales 0000Z, 30Nov 2001 0000Z, 30Nov 2001 Bob Joyce : RSIS, Inc. – PowerPoint PPT presentation

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Title: Bob Joyce : RSIS, Inc.


1
0000Z, 30Nov 2001
Bob Joyce RSIS, Inc. John Janowiak
Climate Prediction Center/NWS Phil Arkin
ESSIC/Univ. Maryland Pingping Xie
Climate Prediction Center/NWS
AMSU
TRMM
SSM/I
2
Two primary types of precipitation algorithms
  • Infrared (GPI, convective-stratiform, OPI)
  • (-) indirect - can only sense cloud-top
    temperature
  • () very good sampling characteristics
    (time space)

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5
Our Approach
  • Use the IR and microwave data but do NOT mix them
  • Use the IR only as a transport and morphing
  • mechanism
  • Here we use precipitation algorithms developed by
  • Ferraro (NESDIS AMSU-B SSM/I) and
  • Kummerow (CSU TRMM) but method is algorithm
  • independent.
  • Enables the generation of spatially and
    temporally
  • complete precipitation fields while maintaining
  • a pure, albeit manipulated, microwave-based
  • analysis

6
Advection vectors are computed from IR for each
2.5ogridbox andall microwave pixels contained in
that grid box are propagated in the direction of
that vector
2.5o
2.5o
7
IR Spatial Correlation Domain for Computation of
Advection Vectors
2.5o
IR (t0)
2.5o
precip
8
Advection Rates for 00Z 30 Nov 2001
. EAST WEST
(pixels/hour)
MERIDIONAL
. NORTH ...SOUTH
(pixels/hour)
9
Actual Microwave Observations
t0
t2 hrs
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13
Validation
14
Initial microwave pass
Next microwave pass
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17
Microwave-Advected
GPCP 1DD
GPI (IR)
18
Potential Applications
  • Real-time quantitative global precipitation
    monitoring
  • Disaster mitigation
  • Provide timely updates for U.S. interests abroad
  • Numerical model initialization validation
  • Improve diurnal cycle in the models
  • Diagnostic studies diurnal cycle in particular

19
Continuing Work
  • Account for precipitation that forms and
    dissipates
  • between microwave overpasses
  • Refine advection vector computation
  • Continue validation effort
  • Test/Include new precipitation products as they
  • become available method is not restricted to
  • particular algorithms or sensors

20
Finis
21
mm/day
Figure 5
22
Microwave propagated by IR
Another test this one is over The South
Atlantic Convergence Zone (SACZ)
Valid time is 1.5 hours after the initial pass
and 6 hours before the next pass
Initial microwave pass
Next microwave pass
Validating microwave data
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24
Spatial Lag Correlation of IR pixel temperature
among nearby 5o x 5o grid boxes to determine
propagation direction
(t 1/2 hr)
(t 0 hr)
5o 12 pixels
5o
5o
5o 12 pixels
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