Noctilucent Cloud observations at Davis

This indicator is no longer maintained, and is considered OBSOLETE. INDICATOR DEFINITION Lidar observations at Davis Station, Antarctica, are used to determine monthly averages of 'percentage of time noctilucent clouds detected' (i.e. total time clouds detected divided by total observing t...

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Bibliographic Details
Other Authors: KLEKOCIUK, ANDREW (hasPrincipalInvestigator), KLEKOCIUK, ANDREW (processor), Australian Antarctic Data Centre (publisher)
Format: Dataset
Language:unknown
Published: Australian Antarctic Data Centre
Subjects:
climatologyMeteorologyAtmosphere
CLOUD FREQUENCY
EARTH SCIENCE
ATMOSPHERE
CLOUDS
CLOUD PROPERTIES
CLOUD HEIGHT
CLOUD VERTICAL DISTRIBUTION
LIDAR
MESOPAUSE
MESOSPHERE
NLC
NOCTILUCENT CLOUD
PMC
POLAR MESOSPEHERIC CLOUD
LIDAR &gt
Light Detection and Ranging
FIXED OBSERVATION STATIONS
CONTINENT &gt
ANTARCTICA &gt
Davis Station
GEOGRAPHIC REGION &gt
POLAR
VERTICAL LOCATION &gt
Antarctic
Davis-Station
Antarc*
Antarctica
Online Access:https://researchdata.ands.org.au/noctilucent-cloud-observations-davis/701757
https://data.aad.gov.au/metadata/records/SOE_NLC
http://nla.gov.au/nla.party-617536
Description
Summary:This indicator is no longer maintained, and is considered OBSOLETE. INDICATOR DEFINITION Lidar observations at Davis Station, Antarctica, are used to determine monthly averages of 'percentage of time noctilucent clouds detected' (i.e. total time clouds detected divided by total observing time, as a percentage), and monthly averages of median altitude of noctilucent clouds. RATIONALE FOR INDICATOR SELECTION Increases in occurrence and spatial extent of noctilucent clouds in the Northern Hemisphere have been linked to cooling of the mesopause region related to enhanced greenhouse warming of the troposphere, and increases in tropospheric methane. Both of these effects have anthropogenic sources. Southern Hemisphere observations of noctilucent clouds are sparse, but potentially provide an independent data set to the Northern Hemisphere observations. A long-term consistent data set is required to determine variations in percentage occurrence and compare this to northern hemisphere observations, particularly as there are subtle differences in the characteristics of the atmosphere in the two hemispheres. Perturbations to the thermodynamics and chemistry of the mesopause region can conceivably be caused by volcanic events and variations in solar activity. Long-term quantification of noctilucent cloud properties will aid in understanding and predicting natural and anthropogenic variability. DESIGN AND STRATEGY FOR INDICATOR MONITORING PROGRAM Spatial scale: Davis Station, Antarctica. Temporal scale: Monthly values. Measurement technique: Lidar (532nm wavelength, minimum altitude resolution 18.7 metres). The raw data used in the analysis of this indicator are obtained from observations by the Davis Lidar in Rayleigh mode. RESEARCH ISSUES changes in the extent and occurrence of noctilucent clouds have implications for the chemistry and climate of the mesopause region. To obtain a more comprehensive picture of the spatial extent of these changes, the underlying physics, and future implications, the Davis observations should be assimilated into research incorporating a diverse body of observations and model predictions. Important additional data will come the remote sensing of temperatures and winds in the mesopause region, from instruments at Davis such as the Czerny-Turner spectrometer, the MF radar and the proposed VHF radar, and other Antarctic measurements.

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