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ISS-Rapid Scatterometer (ISS-RapidScat)

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Status: Current
Mission Category: Other
Launch Date: September 20, 2014
Launch Location: Cape Canaveral Air Force Station

The primary goal of the Rapid Scatterometer (RapidScat) is to provide a gap-filler ocean vector winds measurement capability to mitigate the loss of the NASA Quick Scatterometer (QuikSCAT). Scatterometers are radar instruments that can measure near-surface wind speed and direction over the ocean, and have proved to be extremely valuable for weather forecasting, including hurricane monitoring, and for monitoring large-scale changes in the Earth’s climate, such as El Niño. The RapidScat instrument will be mounted on the International Space Station (ISS) and will provide wind measurements that will enhance the international scatterometer constellation, provide unique cross-calibration capabilities to extend the climate data record initiated by the QuikSCAT satellite. In addition, because of the unique orbit characteristics of the ISS, RapidScat will enable the first measurements of the systematic diurnal changes of winds over the ocean.

RapidScat is sponsored by NASA's Human Exploration and Operations Mission Directorate (HEOMD).

Key ISS-Rapid Scatterometer Facts

Mission/Portal Page: http://www.jpl.nasa.gov/missions/iss-rapidscat/
Launch Vehicle: Space X Falcon 9
Altitude:Distance from sea level. 420km
Inclination: 51.65°
Origination: NASA
Instruments: Rapid Scatterometer
Principle Investigator(s): Ernesto Rodriguez, Ph.D., NASA Jet Propulsion Laboratory, Pasadena, CA, United States

Science Goals:

  • To provide ocean vector wind data for a period of two years to mitigate the loss of QuikSCAT to scientists and weather forecasters.
  • To serve as a calibration standard to the international scatterometer constellation, enabling the continuation of the QuikSCAT data record, and enabling monitoring of climate variability and change over multiple decades.
  • To study the systematic variation of ocean winds as a function of time of day. These variations are important in understanding the dynamics and interactions of the ocean and atmosphere in the tropics, where current climate models still exhibit shortcomings, and which play a significant role in governing the Earth’s energy and water budgets.