High-resolution dynamics limb sounder: Difference between revisions
m →External links: general fixes and stub recategorisation using AWB |
Removing deleted image |
||
Line 1: | Line 1: | ||
{{orphan|date=April 2010}} |
{{orphan|date=April 2010}} |
||
[[Image:Main HIRDLS instrument.jpg|frame|right|High Resolution Dynamics Limb Sounder]] |
<!-- Deleted image removed: [[Image:Main HIRDLS instrument.jpg|frame|right|High Resolution Dynamics Limb Sounder]] --> |
||
'''HIRDLS''': The High Resolution Dynamics Limb Sounder is an instrument on board the [[NASA]] [[Aura (satellite)|Aura]]. It follows in the heritage of LRIR (Nimbus-6), LIMS and SAMS (Nimbus-7), ISAMS and CLAES (UARS). It was designed to observe global distribution of temperature and concentrations of O<sub>3</sub>, H<sub>2</sub>O, CH<sub>4</sub>, N<sub>2</sub>O, NO<sub>2</sub>, HNO<sub>3</sub>, N<sub>2</sub>O<sub>5</sub>, CFC-11, CFC-12, ClONO<sub>2</sub>, and aerosols in the upper troposphere, stratosphere, and mesosphere. |
'''HIRDLS''': The High Resolution Dynamics Limb Sounder is an instrument on board the [[NASA]] [[Aura (satellite)|Aura]]. It follows in the heritage of LRIR (Nimbus-6), LIMS and SAMS (Nimbus-7), ISAMS and CLAES (UARS). It was designed to observe global distribution of temperature and concentrations of O<sub>3</sub>, H<sub>2</sub>O, CH<sub>4</sub>, N<sub>2</sub>O, NO<sub>2</sub>, HNO<sub>3</sub>, N<sub>2</sub>O<sub>5</sub>, CFC-11, CFC-12, ClONO<sub>2</sub>, and aerosols in the upper troposphere, stratosphere, and mesosphere. |
||
Revision as of 11:07, 20 January 2011
HIRDLS: The High Resolution Dynamics Limb Sounder is an instrument on board the NASA Aura. It follows in the heritage of LRIR (Nimbus-6), LIMS and SAMS (Nimbus-7), ISAMS and CLAES (UARS). It was designed to observe global distribution of temperature and concentrations of O3, H2O, CH4, N2O, NO2, HNO3, N2O5, CFC-11, CFC-12, ClONO2, and aerosols in the upper troposphere, stratosphere, and mesosphere.
After launch, activation of the HIRDLS instrument revealed that the optical path was blocked so that 20% of the aperture could view the Earth's atmosphere. Engineering studies suggest that a piece of thermal blanketing material ruptured from the back of the instrument during the explosive decompression of launch. Attempts to remove this material mirror failed. However, even with the 80% blockage, measurements at high vertical resolution can be made at one scan angle.
See also
Template:Space-based meteorological observation
External links