ARM-FIRE Water Vapor Experiment
1 November 2000 - 31 December 2000
Lead Scientist: Henry Revercomb
The Water Vapor Working Group conducted a collaborative effort between NASA and the ARM Water Vapor Working Group (overlapping the Fall SCM IOP) focusing on the accurate measurement of upper tropospheric water vapor.
In addition to the ARM raman lidar and Vaisala RS-80 radiosondes, the following guest instruments were located at the SGP central facility:
- differential absorption lidar (DIAL) from the Max Planck Institute (MPI) in Hamburg, Germany
- scanning raman lidar from the NASA Goddard Space Flight Center (GSFC) in Greenbelt, Maryland
- scanning atmospheric emitted radiance interferometer (AERI) spectrometer from the University of Wisconsin
- Meteolabor "snow white" chilled mirror radiosondes from NASA Langley Research Center (LaRC) in Hampton, Virginia.
In addition to the ground-based instruments, the NASA DC-8 provided an airborne platform for the following instruments:
- differential absorption lidar (LASE) from NASA LaRC
- cryogenic chilled mirror hygrometer from NASA LaRC
- fast-response ozone sensor from NASA LaRC
Scientific hypothesis: 1. Aircraft with continuous profiling capabilities from DIAL, which parallel the ground-based CART Raman lidar capabilities, will be sufficient to handle sampling related problems to compare observations with the Raman lidar and radiosondes.
Coupling the absolute calibration of DIAL with state-of-the- art in-situ sensors is adequate airborne truth
Nighttime Raman lidar has adequate sensitivity and stability to transfer IOP-based aircraft truth to long-term observations and to satellite remote sensing validation. More details are given in the Science Plan.
This field mission experience indicated that it is possible for several sensors to be used in a coordinated fashion over a period of several weeks to achieve a mean water water profile that is accurate at the +/- 5% level using the ARM microwave radiometer (MWR) as the total water column reference. The fall was chosen for this experiment since this is the season that offers the highest probability of clear skies due to the strong frontal passages that occur then. The winter also possesses these strong fronts but the likelihood of snow or ice is much higher in the winter.
AFWEX consisted of both airborne and ground-based instruments. The main result of AFWEX was to demonstrate that, with careful analysis, a core group of 5 instruments was accurate at the 5% level for the profile of water vapor. These 5 instruments were the airborne NASA LaRC LASE water vapor lidar and Diode Laser Hygrometer (DLH), the ground-based Vaisala RS-80H (after application of corrections for time-lag, temperature and total column water), DOE CART Raman Lidar (CARL) and the NASA/GSFC Scanning Raman Lidar (SRL).
A follow-on experiment called AIRS Water Vapor Experiment-Ground (AWEX-G) has been scheduled for (held in) October/November 2003.
Chung ES and BJ Soden. 2009. "A Satellite-Based Assessment of Upper-Tropospheric Water Vapor Measurements during AFWEX." Journal of Applied Meteorology and Climatology, 48(11), 10.1175/2009jamc2250.1.
Field PR, AJ Heymsfield, and A Bansemer. 2007. "Snow Size Distribution Parameterization for Midlatitude and Tropical Ice Clouds." Journal of the Atmospheric Sciences, 64(12), 10.1175/2007jas2344.1.
Baum BA, P Yang, S Nasiri, AK Heidinger, A Heymsfield, and J Li. 2007. " Bulk Scattering Properties for the Remote Sensing of Ice Clouds. Part III: High-Resolution Spectral Models from 100 to 3250 cm ." Journal of Applied Meteorology and Climatology, 46(4), 10.1175/jam2473.1.
Ferrare RA, EV Browell, S Ismail, S Kooi, LH Brasseur, VG Brackett, MB Clayton, J Barrick, GS Diskin, J Goldsmith, BM Lesht, JR Podolske, GW Sachse, FJ Schmidlin, DD Turner, DN Whiteman, D Tobin, L Miloshevich, HE Rivercomb, BB Demoz, and PD Girolamo. 2004. "Characterization of upper-tropospheric water vapor measurements during AFWEX using LASE." Journal of Atmospheric and Oceanic Technology, 21, 10.1175/jtech-1652.1.
Revercomb HE, DD Turner, DC Tobin, RO Knuteson, WF Feltz, J Barnard, J Bösenberg, S Clough, D Cook, R Ferrare, J Goldsmith, S Gutman, R Halthore, B Lesht, J Liljegren, H Linné, J Michalsky, V Morris, W Porch, S Richardson, B Schmid, M Splitt, TV Hove, E Westwater, and D Whiteman. 2003. "The ARM Program's Water Vapor Intensive Observation Periods: Overview, Initial Accomplishments, and Future Challenges." Bulletin of the American Meteorological Society, 84(2), 10.1175/bams-84-2-217.
Miloshevich LM, A Paukkunen, H Vomel, and SJ Oltmans. 2002. Impact of Vaisala Radiosonde Humidity Corrections on ARM IOP Data. In Proceedings of the Twelfth ARM Science Team Meeting, Ed. by D. Carrothers, Richland, WA: U.S. Department of Energy.
Knuteson RO, B Osborne, J Short, HE Revercomb, DC Tobin, and SL Nasiri. 2001. Progress Towards a Characteristic of the Infrared Emissivity of the Land Surface in the Vicinity of the ARM SGP Central Facility: Surface (S-AERI) and Airborne Sensor (NAST-I/S-HIS). In Proceedings of the Eleventh Atmospheric Radiation Measurement (ARM) Science Team Meeting, Ed. by D.A. Carrothers, Richland, WA: U.S. Department of Energy.
Browell EV, S Ismail, and RA Ferrare. 2000. LASE Water Vapor, Aerosol, and Cloud Measurements during Recent Field Experiments. In Tenth ARM Science Team Meeting Proceedings, Ed. by N. Burleigh and D. Carrothers, Richland, WA: U.S. Department of Energy.
View All Related Publications
Campaign Data Sets
|IOP Participant||Data Source Name||Final Data|
|Randall Albertson||DC-8 navigation and mission logs||Order Data|
|J Barrick||Water Vapor||Order Data|
|Jens Boesenberg||DIAL Lidar||Order Data|
|Edward Browell||LASE||Order Data|
|Seth Gutman||GPS||Order Data|
|Barry Lesht||BBSS||Order Data|
|Barry Lesht||DC-8 A/C||Order Data|
|Henry Revercomb||HIS||Order Data|
|Scott Richardson||Chilled Mirror||Order Data|
|G. Sachse||Water Vapor||Order Data|
|Francis Schmidlin||CM Sondes||Order Data|
|David Tobin||NASTI||Order Data|
|David Tobin||NPOESS Aircraft Sounder Testbed - Interferometer||Order Data|
|David Turner||CART scanning raman lidar||Order Data|
|David Turner||MWR-scaled radiosondes||Order Data|
|David Whiteman||GSFC RL||Order Data|