January 25th, 2013
Suomi NPP VIIRS 11.45 Âµm IR images (click image to play animation)
AWIPS II images of 375-meter resolution Suomi NPP VIIRS 11.45 Âµm IR channel data (above; click image to play animation) revealed a surprising amount of sea ice motion in the vicinity of Barrow, Alaska (station identifier PABR) during the 30-hour period between 12:14 UTC on 24 January and 18:30 UTC on 25 January 2013. Large sea ice features with several ice leads and fractures can be seen moving southward against the land-fast ice to the east of Barrow — while to the west of Barrow, strong winds were helping to break the sea ice into smaller ice floes and transport them rapidly westward.
Suomi NPP VIIRS imagery is now being broadcast at the full native 375-meter resolution over the new “POLARSAT” NOAAPORT SBN channel (currently only available for the Alaska Region), for display in the next generation of AWIPS (AWIPS II).
January 24th, 2013
Suomi/NPP VIIRS Visible Image
The Arctic airmass that has overspread the eastern two-thirds of the United States is cold enough that sustained northerly winds down the length of Chesapeake Bay yielded snow showers over extreme southeastern Virginia and northeastern North Carolina. The Suomi/NPP Visible image, above, shows a distinct cloud band over the eastern side of Chesapeake Bay that stretches southwards towards the Outer Banks of North Carolina. Snow was being reported at a number of stations across the Hampton Roads area in southeastern Virginia, with visibility being restricted to 2 miles at Oceana Naval Air Station (KNTU) — and snow was reported as far south as Currituck, North Carolina (KONX).
Bay-effect (or Lake-effect) snows typically occur when the temperature difference between the water surface and lower tropopshere (for example, 850 mb) exceeds about 13 to 15 C. The sounding from Roanoke, VA, from 1200 UTC on 24 January shows temperatures near -12 C at 850 mb. Sea-surface temperatures over the lower Bay are around 5 C. This animation of two MODIS visible images, from 1506 UTC and from 1640 UTC, shows the snow band shifting from the western shore to the eastern shore of the Bay. This event was also caught on radar.
POES AVHRR 0.86 Âµm visible channel and 12.0 Âµm IR channel images
A comparison of 1-km resolution POES AVHRR 0.86 Âµm visible channel and 12.0 Âµm IR channel images at 14:11 UTC or 9:11 AM local time on the morning of 24 January 2013 (above) showed a prominent bay-effect cloud band as it was becoming well-organized over the northern portion of Chesapeake Bay. Cloud top IR brightness temperatures were as cold as -25.5 C (darker blue color enhancement), indicating that the cloud band was almost certainly glaciated. Note the observation of blowing snow (reducing visibility to 2 miles) at Patuxent River Naval Air Station (station identifier KHNK) near the southern end of the cloud band.
The development and movement of the bay-effect snow bands could be seen on 1-km resolution GOES-13 0.63 Âµm visible channel images (below; click image to play animation).
GOES-13 0.63 Âµm visible channel images (click image to play animation)
On the previous day, the 1-km resolution MODIS Sea Surface Temperature (SST) product (below) revealed SST values greater than 40 F or 4.4 C (lighter blue color enhancement) over the central and southern portions of Chesapeake Bay.
MODIS Sea Surface Temperature image
January 23rd, 2013
Suomi NPP VIIRS 0.64 Âµm visible channel images
AWIPS II images of Suomi NPP VIIRS 0.64 Âµm visible channel images (above) showed a very detailed view of “transverse banding” cloud features across parts of northwestern Canada (primarily in northeastern British Columbia) on 23 January 2012. This transverse banding — with the cloud features oriented perpendicular to the flow — is a satellite signature that indicates an increased potential for turbulence. Suomi NPP VIIRS imagery is now being broadcast at full 375-meter resolution over the new “POLARSAT” NOAAPORT channel (currently only available for the Alaska Region), for display in the next generation of AWIPS (AWIPS II).
The corresponding Suomi NPP VIIRS 11.45 Âµm IR channel images are shown below. Cloud top IR brightness temperatures were colder than -60Âº C (dark red color enhancement) in many of the bands.
Suomi NPP VIIRS 11.45 Âµm IR channel images
A comparison of the the VIIRS visible and IR images at 19:05 UTC (11:05 AM local time) are shown below.
Suomi NPP VIIRS 0.64 Âµm visible channel and 11.45 Âµm IR channel images
January 22nd, 2013
Suomi/NPP VIIRS Day/Night Band Imagery (click image to toggle between times)
The Day/Night band on Suomi/NPP produces Night-Time visible imagery using illumination from natural (the moon, forest fires) and man-made sources (city lights, gas flares). Interpretation of the imagery should be done, therefore, with a knowledge of the Lunar phase. In the example above, note the dimming of the clouds over the central plains of the United States between 0752 UTC and 0933 UTC. The 0933 UTC image also shows a gradation in the cloud brightness from east to west — clouds off the west coast of the United States are brighter than clouds over the Plains. The waxing gibbous moon is more than 80% full on 22 January, providing ample light when above the horizon. Moonset occurred over the central USA around 0900 UTC on 22 January; on the West Coast, moonset was closer to 1100 UTC. In the later image, only the regions west of the Rockies are illuminated by the Moon; elsewhere the moon has set, and this is reponsible for the differences in how the clouds are presented.
The 0752 UTC image also contains an excellent example of Moon Glint over the southern Gulf of California. The setting moon is low in the sky, and reflection off the ocean surface is detected.
These images can also be observed using the SSEC Web Map Server. The image below that includes Day/Night Band imagery and Suomi/NPP Tracks was produced with this url.
Suomi/NPP VIIRS Day/Night Band Imagery produced by SSEC WMS