Hurricane Andrew; 1993 Storm of the Century; Tornadoes

We close this part of Section 14 with several special-interest stories.

In late August of 1992, Andrew, a category-five hurricane ripped through the Bahamas, slammed into southern Florida (its eye or center passed over Homestead Air Force Base), and moved into the Gulf of Mexico to hit Louisiana. Although rather small in diameter, this intense storm was the most costly in U.S. history-estimates as high as $30 billion in damage - even though it took just 43 lives (a tribute to the early warning efficacy of metsat monitoring). Winds in excess of 240 km/hr (149 mph) flattened entire housing developments. This devastating hurricane got a lot of attention by a variety of sensors from above and on the ground. Consider these images:

Colorized NOAA-7 image of Hurrican Andrew as it strikes land in Florida.

GOES-7 color composite showing North and South America and the eastern Pacific; a large roundish white cloud in the north-central part of the Gulf of Mexico is Hurricane Andrew approaching landfall near New Orleans.

Color AVHHR closeup view of Andrew over New Orleans.

The top image from NOAA-7 shows the hurricane as it strikes land in Florida, with colorized tones representing higher intensities. In the middle is a GOES-7 full-Earth, color view obtained on August 25, 1992, in which Andrew approaches New Orleans. This perspective indicates scale, showing the hurricane, while powerful as organized, was still just another mass of clouds of no greater extent than some other storm systems. But, on close-up (bottom) in the AVHRR color version (RGB = 0.9; 1.5R; 3.5 µm), the perfection of the eye and the well-developed structure of this counterclockwise-spinning, low-pressure system are obvious.

14-25: What do you think happened to Andrew after it made its second landfall around the Mississippi Delta? ANSWER

The Terra and Aqua programs are the subject of Section 16. These two satellites are not designed specifically as metsats but they do gather considerable data pertinent to weather and climate. Here is a Terra MODIS image of 4 hurricanes (typhoons in the eastern hemisphere) crossing the western Indian Ocean on February 12, 2003:

MODIS image of Indian Ocean typhoons; from left to right - Gerry, Hope, 18s (poorly organized), Fiona.

On March 13, 1993, the "Storm of the Century", shown here in this GOES-7 image, with more intense clouds (color-enhanced), struck the eastern U.S. with massive snow falls and high winds.

Colorized GOES-7 image of the "Storm of the Century," March 13 1993.

The writer (NMS) at the time was in Bloomsburg, Pennsylvania, preparing to leave the next day to give a paper on the Manson Impact Structure (see page 18-2) at the Lunar and Planetary Science Conference in Houston, TX, the first he was to attend since the original Conference on Apollo 11 moon rocks 23 years earlier. It was not to be. Snow locally exceeded 60 cm (24 in), driven into deep banks by winds. All Interstate highways within Pennsylvania closed for two days.

Metsats are excellent monitors of less violent, more conventional, but still interesting weather data. We are all familiar with the passage of cold fronts, followed by clear weather as a pressure high moves in. Commonly, moist, warm air is encountered by the front and develops into a broad area of clouds and often stormy weather. This next image shows the sharp leading edge of a front now off the Atlantic coast of the U.S. and out to sea. At its back edge is another sharp boundary beyond which cold, dry air is moving in.

Passage of a cold front across the Eastern U.S. and onto the Atlantic Ocean.

Lastly, tornadoes, while much more localized than hurricanes or subcontinental storms, can do incredible damage to the areas on which they touch down. Low pressures, and wind velocities that can exceed 200 mph, will flatten buildings (tornadoes have a special fondness for trailer parks), uproot trees, and carry objects for hundreds of feet to even miles from their spot of origin. The storms that brew them are effectively tracked by ground radar and by satellites (usually geostationary). On May 27, 1997 several lines of storm clouds bearing multiple funnel clouds crossed central Texas with deadly results. Here is a GOES-8 image of these advancing fronts.

GOES-8 image of the storm front containing a line of killer tornadoes in a weather front crossing Texas on May 27, 1997.

When a storm has passed and the sky clears, a passing satellite can often see the actual damage if conditions are right. This was the case three days after a killer tornado touched down on May 5, 1999 within Oklahoma City, OK., cutting a path through city and suburbs and just missing the airport. Look for the diagonal blue strip in this IRS-C LISS false color composite - this marks the zone of heavy destruction.

Tornado path (blue diagonal) in Oklahoma City, imaged by the IRS-C LISS.

Now that IKONOS and other high resolution sensors are operational, it is feasible to inspect damage from tornadoes in considerable detail - equivalent to flying an aerial photo mission. A tornado touched down in Fort Worth, TX, ripping off roofs from warehouses and other buildings, as evident in this 1 m resolution IKONOS image.

Damaged buildings in the warehouse district of Fort Worth, TX, following a tornado in 2000; imaged by IKONOS.

The first tornadic storm of 2002 to produce multiple deaths (4) occurred on April 28 around La Plata, Maryland, about 40 miles southeast of Washington. This may have been an F-4 tornado (the second highest wind category) and as such was the most powerful ever to hit Maryland (and one of the strongest ever to hit the East Coast region). Within just two days, the narrow path of destruction (that was, however, 6 miles long) in which several hundred buildings were damaged was imaged by EO-1, as seen here (the pink color was caused by destruction of vegetation [reducing the natural green input]):

EO-1 image of the path of an F-4 tornado that here crosses homes around La Plata, MD.

Still another hazard, and sometimes a killer, associated with usually severe storms are lightning strikes. Worldwide thousands of individual lightning discharges, including dramatic bolts, occur each day.This next map shows the geographic distribution of the frequency of strikes averaged over 5 years (1995-2000) of data collecting by NASA's Optical Transient Detector and by the Lightning Imaging Sensor on TRMM. Note that the central part of Africa has the most lightning strikes; almost all of South America is prone to frequent electrical storm activity.

Global map of frequency of lightning strikes; the areas of greatest number of strikes from 1995 to 2000 are shown in blacks, then reds; lowest blues.