aerisummary

The atmospheric emitted radiance interferometer (AERI) is a ground-based instrument that measures the downwelling infrared radiance from the Earth s atmosphere. The observations have broad spectral content and sufficient spectral resolution to discriminate among gaseous emitters (e.g., carbon dioxide and water vapor) and suspended matter (e.g., aerosols, water droplets, and ice crystals). These upward-looking surface observations can be used to obtain vertical profiles of tropospheric temperature and water vapor, as well as measurements of trace gases (e.g., ozone, carbon monoxide, and methane) and downwelling infrared spectral signatures of clouds and aerosols.

Shortwave elevated air brightness temp. from radiance average (2282_2287 cm-1)
Shortwave radiance average (2282_2287 cm-1) Elevated Air

AWARE (ARM West Antarctic Radiation Experiment)

• Latitude: -77.85011
• Longitude: 166.73011
• Publication Date: 2015-12-01
• Start Date: 2015-12-01
• End Date: 2016-12-29
• Last Updated: 2016-12-31

https://www.arm.gov/connect-with-arm/organization/instrument-mentors/list#aeri

Brian Ermold

Pacific Northwest National Laboratory

Krista Gaustad

Pacific Northwest National Laboratory

Henry Revercomb

University of Wisconsin, Madison

David Turner

NOAA- Earth System Research Laboratory

Raymond Garcia

University of Wisconsin

Denny Hackel

University of Wisconsin

Joe Taylor

University of Wisconsin, Madison

Jonathan Gero

University of Wisconsin

http://dx.doi.org/10.5439/1025146
Atmospheric Radiation Measurement (ARM) user facility. 2015, updated hourly. Atmospheric Emitted Radiance Interferometer (AERISUMMARY). 2015-12-01 to 2016-12-29, ARM Mobile Facility (AWR) McMurdo Station Ross Ice Shelf, Antarctica; AMF2 (M1). Compiled by J. Gero, H. Revercomb, D. Turner, J. Taylor, R. Garcia, D. Hackel, B. Ermold and K. Gaustad. ARM Data Center. Data set accessed at http://dx.doi.org/10.5439/1025146.