ESSA, DMSP, SSM/I; TRMM - Remote Sensing Application - facegis.com
ESSA, DMSP, SSM/I; TRMM

The first U.S. Metsats dedicated to routine operations (rather than, in part, experimental) were the ESSA 1-9 series flown for the Environmental Science Service Administration (formed from the U.S. Coast & Geodetic Survey and the National Weather Service as the predecessor to NOAA which itself was chartered by Congress in 1970 as the umbrella organization that included still other agencies). The ESSA satellite group that began on February 3, 1966, and ended on February 26, 1969 evolved into the current NOAA series. The AVCSs and APTs were the prime sensors.

Hurricanes and cyclones were special targets that ESSA routinely monitored from their early to final stages of development and movement. Here is a view taken on September 1, 1966, of Hurricane Faith as it moved towards Cape Hatteras on the North Carolina coast.

ESSA image of Hurricane Faith, September 1 1966.

The U.S. Air Force program in meteorology, essential to its military operations, began with the launch of the first Defense Meteorological Satellite Program (DMSP) satellite on September 16, 1966. The principal instrument was the Operational Linescan System (OLS), which imaged in the visible and thermal IR (TIR) regions. This program, involving many launches in several series, continues today, and much of its data are declassified. Below is a TIR image of Hurricane Henrietta, spawned in the East Pacific, which struck the west coast of Mexico on September 5, 1995.

DMSP TIR image of HurricanE Henrietta, September 5 1955.

Later DMSPs also carried the Special Sensor Microwave Imager (SSM/I), which measures vertically- and horizontally-polarized radiation at 19.36, 22.23, and 85.5 GHz and horizontally at 37.0 GHz. Here is a global brightness temperature map, derived from Channel 2 data for July 9, 1996:

DMSP SSM/I global brightness temperature map, July 9 1996.

This sensor, a kin to SMMR, detects rainfall and clouds, such as displayed in this world map that shows Total Precipitable Water (in g/cc) as determined from SSM/I data, for September 3, 1987:

Total Precipitable Water map taken from SSM/I data, September 3 1987.

Over the course of a full year, we can average SSM/I readings to provide a global map that summarizes annual rainfall (in millimeters), as presented in this example:

Colored global map of annual rainfall taken from SSM/I data; red is heaviest and purple lightest rainfall.

The first satellite whose primary mission is to measure precipitation is the Tropical Rainfall Mapping Mission (TRMM), a joint research project between the U.S. (NASA) and Japan (National Space Development Agency: NASDA). A basic objective of TRMM is to obtain estimates of the vertical profile of the latent heat (heat resulting from a change of state), released through condensation of water vapor in the atmosphere, especially in the Equatorial Intertropical Convergence Zone (ITCZ). The TRMM is a large spacecraft that a joint engineering team built at NASA's Goddard Space Flight Center and successfully launched from Japan on November 27, 1997. The TRMM Observatory has three primary instruments:

  1. The Precipitation Radar (PR), built in Japan, measures 3-D rainfall distribution. The PR is an electronically scanning radar that operates at 13.8 GHz using horizontal polarization with a 129-slotted waveguide antenna. It has a horizontal resolution of 4.3 km (2.7 mi) at nadir and a scanning swath width of 220 km (137 mi).

  2. The Multi-Channel Microwave Radiometer (TMI), collects data on the integrated-column, precipitation content, its areal distribution, and its intensity. The TMI operates at five frequencies, ranging from 10.65 GHz (45 km [28 mi] spatial resolution) to 85.5 GHz (5 km [3.1 mi] resolution). Dual polarization at four of the frequencies provides nine channels. At a 65 scan angle, the swath width is 760 km (472mi).

  3. The Visible Infrared Scanner (VIRS) provides high resolution (2.1 km [1.3 mi] at nadir) information on cloud cover, cloud type, and cloud top temperatures; being a radiometer it operates at 0.63, 1.6, 3.75, 10.8, and 12.0 mm wavelengths.

In addition, the spacecraft's load includes the Lightning Imaging Sensor (LIS) (at 0.777 mm wavelength) capable of picking out lightning flashes associated with active rainfall and the Clouds and Earth's Radiant Energy System (CERES), a broad-band, scanning radiometer, designed to measure reflected and emitted radiative energy at the surface and for the atmosphere and its constituents.

A goal of this low-altitude (350 km [217 mi]), non-sun-synchronous (precessing) satellite is to provide monthly precipitation data over 500 x 500 km grids, especially for the tropical-ocean regions. A network of ground stations to produce corroborating ground truth is under development. You can find more information and updates on this spacecraft and its products at this NASA Goddard TRMM Home Page.

By December, 1997, the TRMM investigators released the first images on the Internet. We reproduce representative ones here, and you can access others via the above URL. The first compares images over the Hawaiian Islands, obtained simultaneously by TRMM's TMI sensor (left) and the SSM/I on the current DMSP satellite. The improved resolution of the TMI is evident. The islands were largely cloud-covered with localized rainfall (reds).

Comparison of rainfall measurements in the Hawaiian Islands as made by TMI on the TRMM satellite (left) and SSM/I on a DMSP satellite.

The second images show Typhoon Pam in the western Pacific, south of Okinawa in early December. The imaged cloud tops appear gray, and the colors in the flat projection represent relative rainfall intensities. The side view (cross-section) is an extrapolation of data to indicate rain distribution within the cloud mass.

Upper left: TRMM image of developing rainfall system south of Okinawa near Japan; Lower left: For conditions in image above, a calculated distribution of rainfall and clouds; Upper right: TRMM image of a fully developed cyclone near Okinawa; Lower right: For conditions in image above, rainfall and cloud distribution.

TRMM has proved very adept at monitoring the rainfall coming from a hurricane as it is tracked along its path. That is evident in these two views of Hurricane Isabel as it neared the coastline of the eastern U.S. in September, 2003.

Successive stages of Isabel's rainfall.
Cross-sections of Isabel's cloud structure, with rainfall amounts (in mm.) indicated.

TRMM's radar can produce a three-dimensional image of a hurricane's structure, including an indication of cloud heights. Here is a diagram of hurricane Magda off western Australia in January, 2010:

3-D image of Magda's cloud structure.

TRMM can conduct both on-going applied observations that help to monitor rainfall conditions and more scientific studies that are revealing some of the properties of moist atmosphere. Two forms of water exist: Light water (hydrogen has no neutrons) and heavy water (hydrogen has one neutron). Being lighter, the first water type should preferentially migrate further out (up) into the atmosphere. This is observed in this bar graph profile of water in the atmosphere, as measured by TRMM's TES (Thermal Emission Spectrometer). In the rendition, red is heavier isotopic water; blue is lighter. Note the fact that over large water bodies, the heavier water extends to higher elevations in the atmosphere.

TES plot of water with different average weighted light and heavy molecules.

The next image is a composite from several-days coverage showing worldwide rainfall during part of December. Major cloud masses are in white, areas of moderate or intermittent rainfall in purple, and heavier rains in reds, yellows, and greens.

Colored composite TRMM image showing worldwide rainfall during part of December, 1997.

One of TRMM's prime accomplishments is its ability to estimate cumulative rainfall in selected areas over time spans averaged over about a week or longer. In a study of the entire continent of South America for a full year, average rainfalls during that period have been measured using TRMM, Quiksat (a scattering sensor), and GRACE (a geophysical gravity-measuring satellite). The balance between rainfall IN and stream flow OUT was also determined. Here is a smoothed map of rainfall distribution for the month of January, 2004:

Rainfall distribution (generalized) over South America; red denotes higher than average, mauve about average, and blue below average.

Because of its orbital migration, TRMM cannot revisit the same area in shorter (1-2 days) repeats and thus misses some rainfalls associated with thunderstorms, etc.) The Spring of 2003 was very wet in the U.S. Southeast, with a higher than normal number of tornadoes. In this map of rainfall, TRMM determined that up to 16 inches of rain fell in Tennessee and parts of adjacent Alabama and Georgia over a 6 day stretch in early May.

TRMM map showing rainfall totals in a 6 day period in May, 2003 in several southeastern U.S. states.

TRMM continues to determine rainfall amounts over various time interval through August of 2010. Here is a map of rainfall in the Gulf of Mexico over a 7-day stretch, important to those responsible for cleanup after the BP oil spill of 2010:

Rainfall in early August, 2010.

Thus TRMM is well-suited to making measurements that predict parts of the world that are, or will shortly be, experiencing widespread flooding. This composite image shows the magnitude of rainfall within a week in early July 2004 during an exceptionally heavy monsoonal deluge in eastern India, Bangladesh, and the Malayxian Peninsula:

TRMM map of rainfall amounts in eastern India and neighboring regions.

TRMM now has the capability of producing maps that are effective in making flood forecasts. These maps single out (in red below) areas of land that receive 1.5 inches or more in a 24 hour period. They in turn can be used to predict possible flooding conditions at 3 and 7 days after the heavy rainfall. Here is a worldwide rainfall map (>1.5 inches in red) for May 2, 2003:

Areas of the Earth's continents that experienced rainfalls greater than 1.5 inches in a single day, as measured by TRMM.

Source: http://rst.gsfc.nasa.gov