KOMPSAT-5 Satellite Mission Summary

CEOS EO HANDBOOK – MISSION SUMMARY - KOMPSAT-5 -

Full Name

Korea Multi-Purpose Satellite -5
aka Arirang-5

Status

Operational (extended)

Mission Agencies

KARI , TAS-i

Launch Date

22 Aug 2013

Mission Links

mission site

EOL Date

Dec 2024

EO Portal Info

NORAD Catalog #

39227 (TLE)

International Designator

2013-042A

Orbit Type

Sun-synchronous

Orbit Period

98.5 minutes

Orbit Sense

Descending

Orbit Inclination

98.1 deg

Orbit Altitude

550 km

Orbit Longitude

Orbit LST

6:00

Repeat Cycle

28 days

Objectives and Applications

Cartography, land use and planning, disaster monitoring.

Mission Measurements

Category	Parameter	Instrument(s)
Atmosphere	Atmospheric Humidity Fields	AOPOD
	Atmospheric Temperature Fields	AOPOD
Land	Landscape topography	COSI
	Multi-purpose imagery (land)	COSI

Mission Instruments

AOPOD - Atmosphere Occultation and Precision Orbit Determination

COSI - Corea SAR Instrument

OpenSearch Datasets

Selected IDN OpenSearch Results (search all 2 )
CDDIS_SLR_predictions

GPS Radio Occultation Boundary Layer Depth Annual L3 V2 (GPSROZPBLA) at GES DISC $This dataset provides an annual average climatology of planetary boundary layer (PBL) height derived from COSMIC/FORMOSAT-3, TerraSAR-X, KOMPSAT-5, and PAZ Global Positioning System (GPS) radio occultation (RO) measurements. The COSMIC/FORMOSAT-3 mission consists of a six-satellite constellation launched in 2006. Each satellite carries an Integrated GPS Occultation Receiver (IGOR) GPS receiver and is equipped with fore and aft looking antenna to track both setting and rising occultations. The constellation provides globally distributed measurements across different local times. The instrument tracks the L-band microwave signal broadcast by a GPS satellite in a limb-viewing geometry. The IGOR receivers are capable of tracking the GPS signals in open loop through the middle to lower troposphere, which is essential for obtaining data with high quality for PBL height estimation, especially at low latitudes. The refractivity profiles form the basis for this PBL height product. For each occultation, the PBL height is calculated as the height where the vertical gradient of the refractivity (dN/dz) is minimum. This algorithm is designed to locate the height where a large vertical change in refractivity occurs, corresponding to the transition from the free troposphere to the PBL. More details can be found in Ao et al. (2012). This is the latest version of this collection which supercedes previous versions.$

No FedEO OpenSearch datasets found.

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