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Headquarters, Washington
(Phone: 202/358-0836)

Krishna Ramanujan
Goddard Space Flight Center, Greenbelt, Md.
(Phone: 607/273-2561)

Ivy Kupec
Rosenstiel School,
University of Miami
(Phone: 305/421-4704)

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National Oceanic and Atmospheric Administration
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Goddard Space Flight Center, Greenbelt, Md.
(Phone: 301/286-0535)

Other related links:

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Viewable Images

Caption for Item 1: Hurricane Charley, August 10, 2004

TRMM observed Hurricane Charley as it crossed the Caribbean Sea and made landfall on the southwest coast of Florida on August 10. This image shows the horizontal distribution of rain intensity and combines data from TRMM's Precipitation Radar (PR), Microwave Imager (TMI) and Visible Infrared Scanner (VIRS). Credit: NASA/NASDA

High resolution image

For more information about this image and Hurricane Charley visit NASA's Earth Observatory at this link.

Caption for Item 2: Tropical Cyclones Observed by TRMM and Ocean Basins

This graphic shows locations of tropical cyclones observed by TRMM's Microwave Imager instrument during the period from January 1, 1998 to December 31, 2000. Each dot represents one TRMM observation. The solid lines indicate the boundaries of the six ocean basins analyzed in the study. The six basins are: Atlantic (ATL), east-central Pacific (ECPAC), northwest Pacific (NWPAC), north Indian Ocean (NIND), south Indian Ocean (SIND), and South Pacific (SPAC). Credit: Lonfat et al., University of Miami

High resolution image (6.9 MB)

Caption for Item 3: Towering Rain Structures in Hurricane Bonnie, 1998

In 1998, TRMM observed some of the largest chimney clouds seen from above inside Hurricane Bonnie, showing a (cumulonimbus) storm cloud, towering like a skyscraper, 59,000 feet (18 kilometers) into the sky from the eyewall. Credit: NASA/NASDA

High resolution image (10 MB)

Caption for Item 4: Hurricane Floyd Rainfall

The map shows the surface rainfall for Hurricane Floyd on September 13, 1999. The rainfall was measured by TRMM's Microwave Imager instrument. The color coded rain rate is in inches per hour, with blues showing lighter rain and reds indicating higher rainfall. The distance between each circular line growing from the storm's center represents 10 kms. Credit: Naval Research Laboratory, reproduced in Lonfat et al., University of Miami

High resolution image (10 MB)

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August 17, 2004 - (date of web publication)

TRMM SEES RAIN FROM HURRICANES FALL AROUND THE WORLD

 

Hurricane Charley as seen by TRMM

Item 1

 

Since rain and freshwater flooding are the number one causes of death from hurricanes in the United States over the last 30 years, better understanding of these storms is vital for insuring public safety. A recent study funded by NASA and the National Science Foundation offers insight into patterns of rainfall from tropical storms and hurricanes around the world.

Researchers at the University of Miami's Rosenstiel School of Marine and Atmospheric Science, Miami, and the National Oceanic and Atmospheric Administration Atlantic Oceanographic and Meteorological Laboratory's Hurricane Research Division, Miami, used data from NASA's Tropical Rainfall Measuring Mission (TRMM) satellite to show how rain falls at different rates in different areas of a storm. The results were published in the July issue of the journal Monthly Weather Review.

 

This graphic shows tropical cyclones observed by TRMM's Microwave Imager instrument during the period from January 1, 1998 to December 31, 2000.

Item 2

Click on image to enlarge.

The results are already being used in a model developed at the Hurricane Research Division to estimate rainfall accumulation related to tropical cyclones. The findings are important because they may help in the development of better forecasts.

The TRMM satellite offers the best measurements of how and where rain falls around tropical cyclones. This is because its orbit is low to the Earth, allowing more detailed information on storms, and it was designed to cover the tropics.

Tropical cyclones consist of winds rotating around low-pressure centers in the tropics that can develop into everything from tropical storms to Category 5 hurricanes.

 

3d image showing the towering clouds inside of Hurricane Bonnie

Item 3

Click on image to enlarge.
Click here for animation.

From 1998 through 2000, TRMM observed 260 tropical cyclones in six major ocean basins. Researchers found that the rainfall intensity and where the heaviest rains fell varied depending on a storm's wind speeds, its location and the environment of each basin.

Scientists looked at three types of tropical cyclones, based on a standard system for classifying these storms. Tropical storms have wind speeds of less than 73 miles per hour (mph). Category 1 and 2 hurricanes blow with winds of 74 to 110 mph, and Category 3 to 5 hurricanes' winds range above 110 mph.

"This study is important because we know very little about the rainfall distribution in tropical cyclones," said lead author of the study, Manuel Lonfat, a University of Miami researcher. "It revolutionizes our understanding of the distribution of rain in tropical cyclones," he added. Lonfat is a NASA Earth System Science Fellowship recipient.

"More than 50 percent of deaths in the U.S. from tropical cyclones over the last 30 years are related to freshwater flooding. So this is currently a very large problem for the forecasting community," Lonfat said.

 

image showing the rainfall distribution in Hurricane Floyd

Item 4

Click on image to enlarge.

When all storms were averaged together the most intense rainfall occurred within 50 kilometers (about 31 miles) of a storm's center, with evidence of very large rain rates as far as 300 to 400 kilometers (about 186 to 250 miles) from the center.

When all storms were averaged and analyzed basin by basin, storms in the North Indian basin were the wettest, and East-central Pacific storms were the driest. The Atlantic and West Pacific storms showed similar rain rates: this at first surprised the researchers since Western Pacific storms tend to be bigger and were presumed to be wetter.

Researchers also found that the storms were not symmetric, meaning that rain fell at different rates in different areas of a storm. If a round storm were divided into four equal parts through the center, called quadrants, in general it was found that the heaviest rainfall occurred in one of the front quadrants. However, the heaviest rainfall shifted from the front-left to the front-right quadrant as a tropical cyclone's intensity increased.

Tropical storms were less symmetric, while stronger hurricanes had a more symmetric inner core. In the Southern Hemisphere, the heaviest rain occurred to the front-left of the storm's path, while in the Northern Hemisphere the heaviest rainfall peaked in the front-right quadrant.

Normally, the only way to accurately measure rain falling from a hurricane is when it gets close enough to the coast to be picked up by National Weather Service radars, or by rain gages. Since TRMM is space-based, researchers can assess the rainfall over vast tracts of ocean, where these storms spend most of their lives.

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