GOES-11 / GOES-14 / GOES-13 visible channel images

The NOAA GOES-14 satellite (positioned over the Equator at 105º West longitude) was brought out of on-orbit storage for a brief period of testing, beginning on 10 August 2011. A comparison of GOES-11 (GOES-West), GOES-14, and GOES-13 (GOES-East) visible channel images (above) shows the evolution of stratus clouds along the southern California coast and the immediate offshore waters of the Pacific Ocean on 10 August. The images are displayed in the native projection of each GOES satellite, so the cloud features appear slightly different due to the different viewing angles.

On the following day (11 August 2011), multi-panel images show data from all 5 channels of the imager instrument on the GOES-11, GOES-14, and GOES-13 satellites (below). Note that the older GOES-11 imager is the last operational GOES to have the 12.0 µm IR channel — this channel was replaced by the 13.3 µm IR channel on GOES-12 through GOES-15.

GOES-11 imager channel data at 12:45 UTC on 11 August 2011

GOES-14 imager channel data at 13:00 UTC on 11 August 2011

GOES-13 imager data at 13:15 UTC on 11 August 2011

An animation of GOES-14 visible channel images (below) shows the passage of the thunderstorm outflow boundary that ended the long string of 40 consecutive days with daily high temperatures of 100º F or higher at Dallas/Fort Worth, Texas — the high temperature there only reached 97º F on 11 August.

GOES-14 visible channel images centered over Dallas/Fort Worth, Texas

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GOES-13 Visible with Airplane Positions

Turbulence associated with a developing line of convection over the Atlantic Ocean east of Florida was severe enough on August 9th to cause five injuries on a Miami-to-Washington DC flight and force an unscheduled landing of the 737-800 aircraft in Charleston, SC. The GOES-13 image, above, shows the path that the aircraft took through a line of developing convection east of Florida (Click here for a flash-based animation). The time that the satellite was scanning the region east of Florida was between 1935 and 1936 UTC (the nominal time of the image, 1932 UTC, refers to the first line scanned in by GOES-13; it takes almost 5 minutes to completely scan North America. See this NESDIS website for the normal scanning schedule).

Animations of visible imagery, 10.7-micrometer infrared imagery, and 6.5-micrometer infrared imagery (the so-called ‘water vapor channel’) all show a similar evolution, namely strong thunderstorms at the coast of Florida at the start of the loop followed by the development of a line of thunderstorms northeastward. It is through this developing line that the airline penetrated. (The flight path is here).

GOES Satellite data are routinely monitored to detect both the initiation of convection, and the presence of Overshooting Tops and Thermal couplets, the latter two features being well-correlated with severe weather and turbulence. Detection suffers, however, because of the relatively poor spatial and temporal resolution afforded by routine GOES scanning. What was detected on this day?

Overshooting tops were detected over the Florida peninsula at 1715 UTC and at 1732 UTC. The top at 1732 UTC is quite apparent in both the visible and infrared loops. Overshooting tops were not detected in the area again before the turbulence event, but their detection prior to the event suggests an airmass with the potential for strong convective development.

Convective Initiation (CI) was flagged along the southwest-to-northeast line of developing convection at 1832 UTC and 1845 UTC, roughly an hour before the turbulence event. (See this link for all Blog Posts on Convective Initiation). Note that the CI detection in this case — occurring — means that glaciation of the clouds has started. CI is drawing the eye to the convective towers that are growing most rapidly; therefore, their tops cool most quickly. It is to these growing cells that a forecaster must pay attention, particularly when they appear in an environment that will sustain overshooting tops.

(Here is an article on this flight from The Aviation Herald).

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MIMIC Total Precipitable Water (click image to play animation)

The fifth named storm of the Atlantic Tropical season, Emily, is moving towards Hispaniola. The animation of MIMIC Total Precipitable Water (TPW), above, derived from microwave data, shows that Emily is embedded within a region of enhanced moisture (Hurricane Eugene in the eastern Pacific Ocean is also obvious within the TPW loop).

NOAA-18 10.8-micrometer imagery

Morning IR satellite imagery from NOAA-16 and NOAA-18 (above) shows a well-developed central dense overcast (CDO), with some overshooting tops. NOAA-18 recorded cloud-top brightness temperatures as cold as -84 C at 0630 UTC. The NOAA-16 visible image from 1149 UTC also shows overshooting tops.

Emily at 1345 UTC on 3 August (click image to play animation)

Emily is in an environment favorable for slow strengthening. Shear values are modest, oceanic heat content is high and Dry Air is at present displaced from the convection. The projected path over the high terrain of Hispaniola, however, should limit strengthening (and yield very heavy rains over that island).

There have been 5 other tropical systems named Emily in the Atlantic: in 1981, 1987, 1993, 1999 and 2005. The path of 1987’s Emily is — so far — closest to the path of 2011’s Emily. (Historical Hurricane paths are from the Unisys Hurricane page here)

For more information on Emily, version 2011, including its projected path off the east coast of the United States, please see the National Hurricane Center’s website and the CIMSS Tropical Cyclones website.

(Added, later on August 3rd:

GOES-15 visible imagery (click image to play animation)

Persistent shear has displaced the circulation from the convection, as shown in the loop above. Convection continues to develop in the center of the storm, but it does not persist there).

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GOES-13 0.63 µm visible channel images (click image to play animation)

The GOES-R Proving Ground requested that the GOES-13 satellite be placed into Super Rapid Scan Operations (SRSO) mode to monitor the development of Tropical Storm Don as it approached the far southern coast of Texas on 29 July 2011:

Subject: Administrative, GOES-13 (GOES-East) SRSO scheduled for July 29

*Topic*: GOES-13 (GOES-East) SRSO is scheduled for: July 29, 2011

*Correction*: *Product(s) or Data Impacted:* GOES-13 (GOES-East)
Imager Data and Products

*Date/Time Issued*: July 29, 2011 1705 UTC

*Product(s) or Data Impacted:* GOES-13 (GOES-West) Imager Data and
Products

*Date/Time of Initial Impact*: July 29, 2011 J/date 210 1815 UTC

*Date/Time of Expected End*: July 29, 2011 J/date 211 0115 UTC

*Length of Event*: 7 hours

*Impacts on Users and Significance*: Smaller PACUS frame with shortened Southern Hemisphere scan (Southern Hemisphere scan hourly). Increased frequency of images over area of interest (see Details)

*User Actions*: None.

*Details/Specifics of Change*: GOES-R Proving Grounds Testing Over Tropical Storm Don in the Gulf of Mexico at 27 North and 96 West

*Requestor: *CIRA

McIDAS images of GOES-13 0.63 µm visible channel data (above; click image to play animation; also available as a QuickTime movie) showed a number of convective bursts associated with the tropical storm — note that there were several periods where images were available at 1-minute intervals while GOES-13 was in SRSO mode. The ABI instrument on GOES-R will actually be able to provide images as frequently as every 30 seconds over special regions of interest (such as tropical cyclones or severe thunderstorms).

A sequence of three AWIPS images of 1-km resolution MODIS and POES AVHRR IR data (below) displayed intricate cloud top structures and very cold cloud top IR brightness temperatures — as cold as -90ºC (darker violet color enhancement) on the 14:23 UTC MODIS image and the 20:21 UTC POES AVHRR image.

MODIS 11.0 µm and POES AVHRR 10.8 µm IR images

For the three individual 1-km resolution MODIS and POES AVHRR IR images above, comparisons with the corresponding 4-km resolution GOES-13 IR images are shown below. There are slight time differences between the MODIS/AVHRR IR and the GOES-13 IR images — but the majority of the northwestward shift in the location of features on the GOES images is due to parallax.

Even though the spatial resolution of the IR channels on the ABI instrument on GOES-R will be 2-km, these 1-km resolution comparisons still serve to demonstrate that improved spatial resolution should allow better detection of such detailed cloud top structures and cold cloud top IR brightness temperatures associated with tropical cyclones.

08:09 UTC MODIS 11.0 µm IR and 08:15 UTC GOES-13 10.7 µm IR images

14:23 UTC POES AVHRR 10.8 µm IR image and 14:32 UTC GOES-13 10.7 µm IR image

20:21 UTC POES AVHRR 10.8 µm IR image and 20:30 UTC GOES-13 10.7 µm IR image

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