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California Baseline Ozone Transport Study (CABOTS) Group ...
California Baseline Ozone Transport Study (CABOTS) Group Meeting . Date/Time: April 19 (Wednesday) 10:00 am - 2:30 pm PDT Location: ARB CR 510
M10 - Meteomodem
M10 Radiosonde. General description: A radiosonde is a meteorological instrument which, launched under a balloon, measures parameters such as pressure, temperature, humidity and wind (direction, velocity) in the atmosphere and transmits data to the ground. The M10 is the Meteomodem latest generation of radiosonde, operated numerous National Meteorological Services for their upper air station ...
ozone layer | Description, Importance ... - Britannica.com
Ozone layer: Ozone layer, region of the upper atmosphere, between roughly 15 and 35 km (9 and 22 miles) above Earth’s surface, containing relatively high concentrations of ozone molecules. Approximately 90 percent of the atmosphere’s ozone occurs from 10–18 km (6–11 miles) to about 50 km (about 30 miles) above Earth’s surface.
Mauna Loa Observatory - Wikipedia
The Mauna Loa Observatory (MLO) is an atmospheric baseline station on Mauna Loa, on the island of Hawaii
Indian Meteorological Department - Home
METEOROLOGICAL CENTRE, Thiruvananthapuram caters to the meteorological requirements of Kerala and Lakshadweep Islands by supervising and coordinating the weather services in the state.
AN/AMA to AN/ANQ - Equipment Listing
AN/AMQ-1: AM-Modulated Radiosonde; manufactured by Bendix: AN/AMQ-2: Recording Aerograph AN/AMQ-3: Wind Measuring Recording Aerograph; manufactured by Belfort Instrument Co.: AN/AMQ-4
What is a Radiosonde? - Radiosonde Museum of North America
A radiosonde is a small weather station coupled with a radio transmitter. The radiosonde is attached to helium- or hydrogen-filled balloon, called variously a weather balloon or a sounding balloon, and the balloon lifts the radiosonde to altitudes exceeding 115,000 feet.
ozone depletion | Facts, Effects, & Solutions | Britannica.com
Ozone depletion: Ozone depletion, gradual thinning of Earth’s ozone layer caused by the release of chemical compounds containing gaseous chlorine or bromine from industry and other human activities. The thinning is most pronounced in the polar regions, especially over Antarctica.