The map below shows a satellite-derived estimate of temperatures at 4am this morning over the southeastern interior, extending from Fairbanks-land (near the top left) to the Canadian border and western Yukon Territory on the right. The cold conditions of the upper Tanana River valley and the steep valleys of the Fortymile Country and western Yukon are clearly evident, with estimated temperatures around -35°F to -45°F. Ground truth observations provide confirmation: -38°F in Northway this morning, and below -40° in Dawson, but barely below 0°F in Eagle with a breeze blowing.
In recent months I've been working on a project to decode all of the wintertime historical land surface temperature data for Alaska from the MODIS instruments on the Aqua and Terra polar-orbiting satellites. The map above is derived from the realtime MODIS feed, but the entire archive is available from NASA (back to 2000 for Terra and 2002 for Aqua). The full archive is of course a lot of data and takes a long time for my little computer to decode, so I'm only about half way through; but the preliminary results are already quite interesting.
As an example of the kind of analysis that is possible with the data archive, the maps below show the number of days with estimated surface temperatures of -50°F or lower for several winters (November through March). The numbers are conservative estimates, because I've used only "high quality" pixels and there may well have been times when ice fog, cloud cover, or other problems prevented good estimates; but the temperatures are unlikely to be too low and so the counts of days are probably not too high.
Click the images to enlarge. The Old Crow Flats of northern Yukon stand out as remarkably and consistently cold. The results also support Rick's opinion that there are places upriver from Umiat that are quite a bit colder than that notoriously cold place.
Nov 2002 - March 2003:
Thanks for this very interesting work Richard. Seems there is significant climate analysis potential with this kind of analysis. Rick
ReplyDeleteIt would be informative to move the area to the east beyond the Old Crow Flats. Canada is a mystery but much of our weather and climate is influenced by their's.
ReplyDeleteGary
Yes - I hope to expand the analysis to the east after I'm finished with Alaska. The array of grid points (at 750m resolution) is so large that the domain size for simultaneous processing is limited by computer memory.
DeleteThe Old Crow Flats area is a remnant of an earlier lake formed adjacent to the western edge of the Laurentide glaciation:
Deletehttps://www.youtube.com/watch?v=wbsURVgoRD0
http://ecozones.ca/english/region/167.html
Low terrain surrounded by higher ground that supports cold air similar to the Yukon Flats to the SW in Alaska. I wonder if it's an isolated ecoregion or similar to lands to the east?
Your work is appreciated Richard and best wishes for a New Year (and more time and PC processing power?).
Gary
If you're looking for extra computational power this might be worth a look: https://www.worldcommunitygrid.org/climate.action
ReplyDeleteThanks for the link! - I was not aware of this.
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