CIMSS Satellite Blog

03 August 2008 marked the 22nd  consecutive day of daily high temperatures of 90º F or higher at Denver, Colorado (the old record was 18 consecutive days, set back in 1874 and 1901). AWIPS images of the MODIS Land Surface Temperature (LST) product (above) revealed daytime LST values as high as 140º F in southeastern Colorado and 134º F in southwestern Nebraska — while the surface “skin temperatures” were quite warm, the actual air temperatures (measured within shaded instrument shelters located about 5  feet above the surface) were only the in upper 90s to low 100s F.

It is interesting to note that the LST values were significantly lower across much of southcentral and southeastern Nebraska (in the upper 80s to low 90s F, green to yellow colors), even though the air temperatures were similar to those seen in eastern Colorado at that time (in the upper 90s to low 100s F).  These lower LST values were due to a much higher density of vegetation in eastern Nebraska, as shown by a comparison with the MODIS Normalized Difference Vegetation Index (NDVI) product (below) — NDVI values were greater than 0.7 in Nebraska, compared to 0.1 to 0.3 across much of eastern Colorado. In addition, very dry conditions had prevailed across eastern Colorado — Denver had only received 3.28 inches of precipitation so far in the year (the normal is 10.25 inches for the 01 January  - 31 July period) — in contrast with Hastings in eastern Nebraska, which had received 6.77 inches of precipitation so far in the year (the normal precipitation is 3.81 inches for the 01 January - 31 July period). The combination of drier soils and sparse vegetation  helped contribute to such high MODIS LST values.

MODIS true color imagery from the SSEC MODIS Today site (below) confirmed the presence of a much higher density of vegetation (denoted by darker green colors) across eastern Nebraska, compared to that found across eastern Colorado.

Given the rather large satellite viewing angle (or “zenith angle”) of geostationary satellites positioned over the Equator, one would think that the imagery would not be of much value over places such as far northern Alaska. However, a forecast discussion issued by Fairbanks, Alaska mentioned the utility of GOES visible imagery for monitoring fog and stratus along western parts of the Arctic coast of Alaska:

NORTHERN ALASKA FORECAST DISCUSSION
NATIONAL WEATHER SERVICE FAIRBANKS AK
347 AM AKDT SAT JUL 5 2008

.DISCUSSION…

OVER THE ARCTIC…GOES VIS LOOP SHOWING AN EXTENSIVE AREA OF STRATUS OVER AREAS FROM BARROW NORTH THROUGH SOUTHWEST…INCLUDING MOST OF ZONE 201. THIS STRATUS IS MISSED BY THE LOW LEVEL RH PROGS ON BOTH THE GFS AND NAM MODELS. THIS AREA IS LIKELY TO REMAIN FOGGY THROUGH TONIGHT WITH ONSHORE FLOW CONTINUING…ALTHOUGH VISIBILITY MAY COME UP SOME DURING THE AFTERNOON AND EARLY EVENING. DENSE FOG HEADLINES WILL BE POSTED FOR ZONES 201 AND 202. THE EASTERN ARCTIC COAST IS LIKELY TO REMAIN FOG-FREE.

GOES-11 visible imagery at 30-minute intervals on 05 July 2008 (above) does indeed do a fairly good job of showing the movement of the bank of fog and stratus that had moved inland over locations such as Barrow (PABA), Wainwright (PAWI), and Point Lay (PLIZ) during the day. A surface meteorogram for Wainwright, Alaska (below) shows that the surface visibility remained at or below 1 mile during much of that particular day, and temperatures dropped below freezing as onshore winds persisted.

Other features of interest to note on the GOES-11 visible imagery shown above:

1. a long smoke plume from a wildfire, which originates just southeast of Fort Yukon (PFYU) and blows southwestward across central Alaska
2. the high amount of sea ice that remained in the Arctic Ocean north of Alaska
3. the snow-covered mountains of the Alaska Range in the southern part of the state — between Minchumina (PAMH) and Talkeetna (PATK) — which includes the summit of Mount McKinley (Denali) at 20,320 feet (6,194 m)
4. northern Alaska experiences 24 hours of continuous daylight during this part of the summer