tovs path-p
DESCRIPTION
TOVS Path-P. Axel Schweiger Polar Science Center University of Washington (Given by Jeff Key , NOAA/NESDIS, Madison). Path-P is a derivative of Path-B with polar modifications Processed north of 60 N, 1979-2004, 100 km grid, daily, monthly - PowerPoint PPT PresentationTRANSCRIPT
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TOVS Path-P
• Path-P is a derivative of Path-B with polar modifications
• Processed north of 60 N, 1979-2004, 100 km grid, daily, monthly
• Temperature and humidity profiles, cloud fraction, cloud height
Axel SchweigerPolar Science Center
University of Washington
(Given by Jeff Key, NOAA/NESDIS, Madison)
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Current Path-P Activities• Compilation of Collocation Data Set (1979-2004)
– Radiosondes (multiple data sets)– EECRA (surface cloud observations, 1979-1996)– Lidar/Radar cloud obs. from (SHEBA, Barrow, SGP)– Snow and Ice Charts (NSIDC) – HIRS/MSU (Brightness Temperatures)– Area N40 + SGP, possible future expansion
• Rework of cloud algorithm– Adjustment of thresholds, validation– Additional tests (e.g. 7.2 -11 μm after Liu et. al. )
• Recomputation of Radiance Bias Adjustments• Eventual reprocessing• Will allow point by point comparison of surface cloud observations
with HIRS/MSU-derived.
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TPP and APP-X
WinterDJF
SpringMAM
-4 %/dec -7%/dec
+5%/dec +4%/dec
1980 2001 1980 2001
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TPP and APP-X 1980-2001 (1982-1999)
SummerJJA
FallSON
1980 2001 1980 2001
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APP-X vs. TOVS Path-P: JJA, Beaufort Sea
AP
P-X
TOVS Path-P (From J. Francis)
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ERA-40 Winter (DJF) Total Cloud Fraction (1980-2001)
Trend
%/decade
57 01
12%/decade
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ERA-40 and TPP Cloud Fraction Spring (MAM)
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ISCCP D1 TOVS Path-P
Summer
Winter
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ISCCP D1 Clear Sky Composite vs Surface Obs
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