Ground-Based Lidar Measurements of Aerosols During ACE-2: Instrument Description, Results, and Comparisons with Other Ground-Based and Airborne Measurements
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Authors
Welton, Ellsworth J.
Voss, Kenneth J.
Gordon, Howard R.
Maring, Hal
Smirnov, Alexander
Holben, Brent
Schmid, Beat
Livingston, John M.
Russell, Philip B.
Durkee, Philip A.
Advisors
Second Readers
Subjects
OPTICAL RADAR
AEROSOLS
VERTICAL DISTRIBUTION
HORIZONTAL DISTRIBUTION
SAHARA DESERT (AFRICA)
METEOROLOGICAL INSTRUMENTS
RADAR MEASUREMENT
BACKSCATTERING
OPTICAL THICKNESS
WEATHER STATIONS
CALIBRATING
DISSIPATION
DUST
ATMOSPHERIC COMPOSITION
CANARY ISLANDS
AEROSOLS
VERTICAL DISTRIBUTION
HORIZONTAL DISTRIBUTION
SAHARA DESERT (AFRICA)
METEOROLOGICAL INSTRUMENTS
RADAR MEASUREMENT
BACKSCATTERING
OPTICAL THICKNESS
WEATHER STATIONS
CALIBRATING
DISSIPATION
DUST
ATMOSPHERIC COMPOSITION
CANARY ISLANDS
Date of Issue
2000-01
Date
Jan 01, 2000
Publisher
Language
Abstract
A micro-pulse lidar system (MPL) was used to measure the vertical and horizontal distribution of aerosols during the Aerosol Characterization Experiment 2 (ACE-2) in June and July of 1997. The MPL measurements were made at the Izana observatory (IZO), a weather station located on a mountain ridge (28 deg 18 min N, 16 deg 30 min W, 2367 m asl) near the center of the island of Tenerife, Canary Islands. The MPL was used to acquire aerosol backscatter, extinction, and optical depth profiles for normal background periods and periods influenced by Saharan dust from North Africa. System tests and calibration procedures are discussed, and an analysis of aerosol optical profiles acquired during ACE-2 is presented. MPL data taken during normal IZO conditions (no dust) showed that upslope aerosols appeared during the day and dissipated at night and that the layers were mostly confined to altitudes a few hundred meters above IZO. MPL data taken during a Saharan dust episode on 17 July showed that peak aerosol extinction values were an order of magnitude greater than molecular scattering over IZO, and that the dust layers extended to 5 km asl. The value of the dust backscatter-extinction ratio was determined to be 0.027 +/- 0.007 sr(exp -1). Comparisons of the MPL data with data from other collocated instruments showed good agreement during the dust episode.
Type
Article
Description
The article of record as published may be found at http://dx.doi.org/10.1034/j.1600-0889.2000.00025.x
Series/Report No
Department
Organization
Ames Research Center
Identifiers
NPS Report Number
Sponsors
Funding
NCC2-1094
Format
Citation
Tellus; p. 636-651; (ISSN 0280-6509); Volume 52B; No. 2
Distribution Statement
Approved for public release; distribution is unlimited.
Rights
This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.
