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MSG Battlespace Products Including Icing. Stan Kidder. Purpose of Seminar. To update the Meteosat Second Generation (MSG) products reported at the last annual review (Adelphi, 15-17 Nov 2005) To demonstrate application of the products to a current battlespace
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MSG Battlespace Products Including Icing Stan Kidder
Purpose of Seminar • To update the Meteosat Second Generation (MSG) products reported at the last annual review (Adelphi, 15-17 Nov 2005) • To demonstrate application of the products to a current battlespace • To outline future work to improve the products
The Battlespace • Resources, such as MSG data, • Need to be applied quickly
The Battlespace • Resources, such as MSG data, • Need to be applied quickly • To the Battlespace, which can be anywhere
Products To Be Discussed MSG Cloud Product 10.8 µm Brightness Temperature Dust Product Precipitating Cores Skin Temperature Cloud Mask Cloud Phase / Icing
Web Link • Connect to this link if you can, but it is not necessary http://products.cira.colostate.edu/MSG/Mideast • If you connect (now or later) you will see something like this:
Warning! • The products displayed on the Web site are experimental, non-operational products which can change at any time. • The site will soon be passworded. If you would like to continue viewing it, please send me email: kidder@cira.colostate.edu
Daytime MSG Cloud Product • (Red, Green, Blue) = 255*(A1.6, A0.8, A0.6) • Liquid water clouds are highly reflective at all three wavelengths and therefore appear white • Ice clouds are highly reflective at 0.8 and 0.6 µm, but poorly reflective at 1.6 µm. They therefore appear cyan in the resulting image.
Nighttime MSG Cloud Product • 3.9 µm albedo • Liquid water clouds are reflective at 3.9 µm and therefore appear white • Thin ice clouds transmit radiation from below and therefore appear to have a negative albedo (and are black in the imagery) • Some soils (northern Sinai) are bright as is thick cirrus
10.8 µm Brightness Temperature • A standard product—one of several products that a forecaster might want to look at to interpret the scene • Clouds colder than −20°C are colored in 10 K increments
Dust Product • EUMETSAT Product • R=T12.0 – T10.8G=T10.8 – T8.7 B=T10.8 • Dust is pink and moves • Low clouds, unfortunately, are also pink and they move • Thin cirrus is blue • Thick cirrus is dark red
Precipitating Cores • Identifies deep, cold clouds which are likely to be precipitating. • Water vapor is used to screen out low clouds • Precipitation clouds (green) are those for which T10.8 – T6.2 < 11 K (an empirically determined threshold).
Skin Temperature • Uses the algorithm of Price (1984), modified for MSG channels • Tskin = T10.8 + 2.5 (T10.4 – T12.0)
Cloud Mask • Uses 8.7 µm channel • The warmest pixel in the previous 10 days is used as a background • Pixels colder than the background are cloudy • Over land, DT = 8 K • Over water, DT = 4 K • Some clouds are missed
Cloud Phase / Icing • Starts with the 8.7 µm cloud mask • Ice clouds (white) are those for which • T10.8 < −30°C (day or night) or • Clouds are “cyan” in MSG Cloud Product (day) • Clouds are “black” in MSG Cloud Product (night)
Cloud Phase / Icing • All clouds which are not ice clouds are liquid water clouds • Warm liquid water clouds (>0°C, yellow) are safe to fly in • Cold liquid water clouds (≤0°C, red) represent an icing hazard This product needs work. Some clouds are missed, and some are incorrectly typed.
Future Work • CloudSat and CALIPSO offer a golden opportunity to verify these (or any) cloud algorithms.
MODIS Imagery CloudSat and CALIPSO ground track
CALIPSO Imagery Cirrus Mid-level Clouds North South MODIS Image
CloudSat Imagery Mid-level Clouds MODIS Image
Summary & Conclusions • A set of cloud products using MSG data was developed quickly to support a current battlespace (I started work on this project on 24 Aug 2006) • Development of the products reveals deficiencies in current algorithms • CloudSat and CALIPSO data offer a way forward