GOES-13 and GOES-12 visible images (centered over Tampa, Florida)

The GOES-12 satellite (which had experienced a thruster anomaly back on 14 December 2008) was re-activated on the morning of 05 January 2009 (beginning at 15:15 UTC). A comparison of GOES-13 and GOES-12 visible images (above) centered on Tampa, Florida showed that the GOES-12 image navigation was initially a bit “shaky”, but seemed to stabilize after a couple of hours. The NOAA/NESDIS Office of Satellite Operations (OSO) and Office of Satellite Data Processing and Distribution (OSDPD) will continue to monitor the performance of GOES-12 during the Image and Navigation  Recovery (INR) period, before the decision is made to re-establish GOES-12 as the operational GOES-East satellite (possibly on the morning of 06 January 2009?).

For the latest information, see the NOAA Satellite Services Division Special Bulletins.

— 06 JANUARY UPDATE —

As of 15:15 UTC on 06 January 2008, GOES-12 has resumed duty as the operational GOES-East satellite.

GOES-12 visible image

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MODIS visible, snow/ice, and IR window channel images

A freezing drizzle / light freezing rain event occurred across parts of the Upper Midwest on 03 January – 04 January 2009 — an ice accrual of 0.1 to 0.2 inch was reported at some locations in northern Iowa, southern Minnesota, and southern Wisconsin. Post-event AWIPS images of the 1-km resolution MODIS visible channel, the 2.1 µm  “snow/ice” channel, and the 11.0 µm “IR window” channel (above) demonstrated the utility of using the snow/ice channel imagery to depict the areal coverage of significant ice accrual. Snow (and especially ice) are strong absorbers at the near-IR 2.1 µm wavelength, so those show up as much darker features on the MODIS snow/ice image (in contrast to supercooled water droplet clouds, which show up as much brighter features).

A mixture of low and high clouds covered  the southern, southeastern, and eastern portions of satellite images shown above — but most of the MODIS image scene on 04 January was cloud-free snow cover. Even though there was generally more snow cover in place across the northern half of the image area (from eastern South Dakota to northern Minnesota), the ice-glazed snow pack farther to the south across norther Iowa and southern Minnesota appeared even darker on the snow/ice image.

The National Weather Service forecast office at Milwaukee/Sullivan, Wisconsin posted an excellent  discussion of the classic thermal profile for ice for this particular event.

— 05 JANUARY UPDATE —

On the following day (05 January), conditions were relatively cloud-free over most of the region, allowing a view of the ice accrual farther to the east across southern Wisconsin (below). The western half of the darker “ice accrual signal” over western Iowa seemed to be diminishing, due to full sunshine and brisk southwesterly winds helping to erode the thickness of the surface ice glaze somewhat. MODIS Land Surface Temperatures were in the upper 20s to around 30 F (darker green colors) across the ice-covered areas of northern Iowa at 17:30 UTC (11:30 am local time).

MODIS visible, 2.1 µm snow/ice, and Land Surface Temperature images

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GOES-13 fog/stratus product

AWIPS images of the GOES-13 fog/stratus product (above) showed a plume of advection fog curling northwestward across southern Oklahoma on 02 January 2009. A relatively moist low-level air mass with dew points in the 40s F was flowing from northeastern Texas into southeastern Oklahoma (where radiational cooling was allowing surface air temperatures to drop into the upper 30s F). Once the fog moved in, the surface visibility was restricted to 1/4 mile at Ardmore (station identifier KADM) and Stillwater (station identifier KSWO) in Oklahoma.

GOES-13 fog/stratus product + NAM surface winds

A sequence of GOES-13 fog/stratus product images with an overlay of the surface frontal analysis and the NAM20 surface winds (above) indicated that there was a weak surface low located over northern Texas, which was helping to feed the moisture across the decaying stationary frontal boundary and into Oklahoma.

GOES-13 sounder Cloud Top Height product

Images of the GOES-13 sounder Cloud Top Height product (above) indicated that the cloud tops were generally in the 7500-8000 foot range (yellow to light green colors) across southeastern Oklahoma.

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MTSAT High Density Winds (AWIPS menu)

TECHNICAL IMPLEMENTATION NOTICE 08-61
NATIONAL WEATHER SERVICE HEADQUARTERS WASHINGTON DC
317 PM EDT FRI AUG 1 2008 

SUBJECT:  NESDIS HIGH DENSITY GEOSTATIONARY WINDS TO BE
          ADDED TO SBN/NOAAPORT: EFFECTIVE OCTOBER 15 2008 

EFFECTIVE WEDNESDAY OCTOBER 15 2008...BEGINNING AT APPROXIMATELY
1500 COORDINATED UNIVERSAL TIME /UTC/...THE NATIONAL
ENVIRONMENTAL SATELLITE...DATA...AND INFORMATION SERVICE /NESDIS/
AND NWS START DISSEMINATING HIGH DENSITY GEOSTATIONARY /MTSAT/
WIND PRODUCTS VIA SBN/NOAAPORT.

THE MTSAT WINDS /FROM THE JAPANESE SATELLITE/ WILL AUGMENT THE
CURRENT GOES EAST AND WEST HIGH DENSITY WINDS OVER SPARSE DATA
REGIONS...MOST BENEFITING THE ALASKA AND PACIFIC REGIONS AND THE
AVIATION WEATHER CENTER /AWC/.

Coverage of MTSAT High Density Winds vs GOES High Density Winds

A comparison of the areal coverage of the MTSAT vs the GOES high density winds is shown on the Pacific Mercator scale  (above) and Northern Hemisphere scale (below). The MTSAT high density winds will be available north of the Equator every 3 hours (at 02, 05, 08, 11, 14, 17, 20, and 23 UTC), and south of the Equator every 6 hours (at 00, 06, 12, and 18 UTC).

Coverage of MTSAT High Density Winds vs GOES High Density Winds

With the AWIPS cursor sampling function activated, the user will be able to display the valid time, the type of satellite imagery used to derive a particular AMV (Visible, InfraRed, shortwave InfraRed, or Water Vapor), the pressure of the height assignment for that AMV, and the direction/speed of that AMV (below). The wind vectors can be color-coded according to pressure layers (as shown below), or by AMV type (IR, Water Vapor, Visible, or 3.9 µm shortwave IR). Targets are tracked on three consecutive satellite images in order to calculate the direction and speed of each AMV.

MTSAT High Density Winds

These MTSAT winds available on AWIPS should be very similar to those derived using GOES data, since NESDIS is using the same AMV software (which was developed at CIMSS) for both satellites. For more details about the derivation and application of satellite-derived atmospheric motion vector products, see the SHyMet GOES High Density Winds lesson.

Reference:

Velden, C.S. et al., 2005: Recent Innovations in Deriving Winds from Meteorological Satellites. Bull. Amer. Meteor. Soc., 86, 205-223

– Updated 29 January 2009 –

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