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NOAA
NESDIS
January 8, 1999 |
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This is evident in both the 3.7 micrometers (Figure 2) and 10.8 micrometers
(Figure 3) AVHRR imagery as well as the GOES imagery at that time.
In Figure 4, note the cyan colors over the western portion of Hudson
Bay corresponding to roughly -15 degrees Celsius next to the red
colors corresponding to roughly -3 degrees Celsius.
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Figure 5 10.8 Micrometers |
Figure 6 10.8 Micrometers |
Figure 5 shows the temperature observations for the region. The coldest area shown in this image is in the western portion of Hudson Bay which would support ice development over the Bay. Figure 6 shows the same imagery using a special enhancement table to focus on the warmer water temperatures adjacent to the ice in the western portion of Hudson Bay.
In summary, the satellite data (AVHRR and GOES-8) data is used in conjunction with surface observations to estimate the ice coverage in the western portion of Hudson Bay. The AVHRR imagery provided a better view of the area than the the GOES, however, the GOES imagery had better time continuity. Together, the POES and GOES satellites provide data to compliment each other.
We welcome your comments and discussion at ramsdis@comet.ucar.edu
| Information Contact: Lewis Grasso | |
| CIRA/RAMM WebMaster: Roger Phillips | |
| Author: Dan Bikos | |
| Last Updated: January 8, 1999 |