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If imagery is zoomed in at an adequate range, actual weather satellite data can be superimposed. VIPIR images can be constructed from multiple sources, including Doppler weather radar and NEXRAD. [3] It is used by television meteorologists to give a comprehensive view of weather, in particular severe weather events.
Crotalus cerastes, known as the sidewinder, horned rattlesnake or sidewinder rattlesnake, [3] is a pit viper species belonging to the genus Crotalus (the rattlesnakes), and is found in the desert regions of the Southwestern United States and northwestern Mexico.
The optimal use of satellite data in climate and global change studies has become another essential part of the CIMSS mission. CIMSS serves as an international center for research on the interpretation and uses of operational and experimental satellite observations and remote sensing data acquired from aircraft and the ground.
After experiencing several delays, the launch of the COSMIC satellite constellation atop a Minotaur launch vehicle from Vandenberg AFB occurred at 01:40 GMT, on 15 April 2006, despite heavy fog. [2] The satellites, which orbit at an altitude of 500 miles, required over a year to move into the correct positions to provide full global coverage.
Artist illustration of the NOAA-20 Satellite. The Joint Polar Satellite System (JPSS) is the latest generation of U.S. polar-orbiting, non-geosynchronous, environmental satellites. JPSS will provide the global environmental data used in numerical weather prediction models for
The low-rate picture transmission (LRPT) is a digital transmission system, intended to deliver images and data from an orbital weather satellite directly to end users via a VHF radio signal. It is used aboard polar-orbiting, near-Earth weather satellite programs such as MetOp and NPOESS .
Sidewinding in a newborn sidewinder rattlesnake. Yellow regions are lifted above the sand and in motion at the time of the photo, while green regions are in static contact with the sand. Blue denotes tracks. Scale imprints are visible in the tracks, showing that the snake's body is static during ground contact. Tracks of a sidewinder in the sand.
[1] The albedo of these low level clouds is much higher than the albedo of the underlying ocean surface and correctly modeling these clouds is needed to limit the uncertainty in climate model predictions. The remote sensing of the planetary boundary layer, especially clouds and aerosols within the planetary boundary layer can help verify and ...