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TitleSPARC: new cloud, snow, and cloud shadow detection scheme for historical 1-km AVHHR data over Canada
 
AuthorKhlopenkov, K V; Trishchenko, A PORCID logo
SourceJournal of Atmospheric and Oceanic Technology vol. 24, issue 3, 2007 p. 322-343, https://doi.org/10.1175/JTECH1987.1 Open Access logo Open Access
Image
Year2007
Alt SeriesEarth Sciences Sector, Contribution Series 2005700
PublisherAmerican Meteorological Society
Documentserial
Lang.English
Mediapaper; on-line; digital
File formathtml; pdf
SubjectsNature and Environment
ProgramReducing Canada's Vulnerability to Climate Change
AbstractThe identification of clear-sky and cloudy pixels is a key step in the processing of satellite observations. This is equally important for surface and cloud-atmosphere applications. In this paper, we present the SPARC (Separation of Pixels using Aggregated Rating over Canada) algorithm, a new method of pixel identification for image data from the Advanced Very High Resolution Radiometer (AVHRR) onboard the NOAA satellites. The SPARC algorithm separates image pixels into clear-sky and cloudy categories based on a specially designed rating scheme. A mask depicting snow/ice and cloud shadows is also generated. The SPARC algorithm has been designed to work year round (day and night) over the temperate and polar regions of North America, for current and historical AVHRR/NOAA High-Resolution Picture Transmission (HRPT) and Local Area Coverage (LAC) data with original 1-km spatial resolution. The algorithm was tested and applied to data from the AVHRR sensors flown onboard NOAA-6 to NOAA-18. The method was employed in generating historical clear-sky composites for the 1982-2005 period at daily, 10-day and monthly time-scales at 1-km resolution for an area of 5700×4800 square km centered over Canada. This region also covers the northern part of the United States including Alaska, as well as Greenland and the surrounding oceans.
The SPARC algorithm is designed to produce an aggregated rating that accumulates the results of several tests. The magnitude of the rating serves as an indicator of the probability for a pixel to belong to clear-sky, partly cloudy or overcast categories. The individual tests employ the spectral properties of 5 AVHRR channels, as well as surface the skin temperature maps from the North American Regional Reanalysis (NARR) dataset. These temperature fields are available at 32×32 square km spatial resolution and at 3 hour time intervals. Combining all test results into one final rating for each pixel is beneficial for the generation of multi-scene clear-sky composites. The selection of the best pixel to be used in the final clear-sky product is based on the magnitude of the rating. This provides much improved results relative to other approaches or "yes/no" decision methods.
The SPARC method has been compared to the results of supervised classification for a number of AVHRR scenes representing various seasons (snow-free summer, winter with snow/ice coverage and transition seasons). The results show an overall agreement between the automated (SPARC) and the supervised classification at the level of 80 % to 91 %.
GEOSCAN ID221765

 
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