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AGU: Journal of Geophysical Research, Atmospheres

 

Index Terms

  • Atmospheric Composition and Structure: Aerosols and particles
  • Atmospheric Composition and Structure: Geochemical cycles
  • Atmospheric Composition and Structure: Transmission and scattering of radiation
  • Atmospheric Composition and Structure: Troposphere—constituent transport and chemistry
Abstract
Cited By (30)
 

Abstract

Analysis of measurements of Saharan dust by airborne and ground-based remote sensing methods during the Puerto Rico Dust Experiment (PRIDE)

Jeffrey S. Reid

Space and Naval Warfare Systems Center-San Diego, San Diego, California, USA

Naval Research Laboratory, Monterey, California, USA

James E. Kinney

Space and Naval Warfare Systems Center-San Diego, San Diego, California, USA

Douglas L. Westphal

Naval Research Laboratory, Monterey, California, USA

Brent N. Holben

NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

Ellsworth J. Welton

NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

Si-Chee Tsay

NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

Daniel P. Eleuterio

Naval Postgraduate School, Monterey, California, USA

James R. Campbell

Science Systems and Applications, Inc., Greenbelt, Maryland, USA

Sundar A. Christopher

Department of Atmospheric Sciences, University of Alabama, Huntsville, Alabama, USA

P. R. Colarco

Laboratory for Atmospheric and Space Physics, Program in Atmospheric and Oceanic Sciences, University of Colorado, Boulder, Colorado, USA

Haflidi H. Jonsson

Naval Postgraduate School, Monterey, California, USA

John M. Livingston

SRI International, Menlo Park, California, USA

Hal B. Maring

Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida, USA

Michael L. Meier

Material Science and Chemical Engineering, University of California, Davis, California, USA

Peter Pilewskie

NASA Ames Research Center, Mountain View, California, USA

Joseph M. Prospero

Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida, USA

Elizabeth A. Reid

Naval Research Laboratory, Monterey, California, USA

Lorraine A. Remer

NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

Philip B. Russell

NASA Ames Research Center, Mountain View, California, USA

Dennis L. Savoie

Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida, USA

Alexander Smirnov

University of Maryland Baltimore County, Baltimore, Maryland, USA

Didier Tanré

Laboratoire d'Optique Atmospherique, CNRS Universite des Sciences et Technologies de Lille, Villeneuve d'Ascq, France

For 26 days in mid-June and July 2000, a research group comprised of U.S. Navy, NASA, and university scientists conducted the Puerto Rico Dust Experiment (PRIDE). In this paper we give a brief overview of mean meteorological conditions during the study. We focus on our findings on African dust transported into the Caribbean utilizing a Navajo aircraft and AERONET Sun photometer data. During the study midvisible aerosol optical thickness (AOT) in Puerto Rico averaged 0.25, with a maximum >0.5 and with clean marine periods of ∼0.08. Dust AOTs near the coast of Africa (Cape Verde Islands and Dakar) averaged ∼0.4, 30% less than previous years. By analyzing dust vertical profiles in addition to supplemental meteorology and MPLNET lidar data we found that dust transport cannot be easily categorized into any particular conceptual model. Toward the end of the study period, the vertical distribution of dust was similar to the commonly assumed Saharan Air Layer (SAL) transport. During the early periods of the study, dust had the highest concentrations in the marine and convective boundary layers with only a weak dust layer in the SAL being present, a state usually associated with wintertime transport patterns. We corroborate the findings of Maring et al. [2003] that in most cases, there was an unexpected lack of vertical stratification of dust particle size. We systematically analyze processes that may impact dust vertical distribution and speculate that dust vertical distribution predominately influenced by flow patterns over Africa and differential advection coupled with fair weather cloud entrainment, mixing by easterly waves, and regional subsidence.

Received 29 April 2002; accepted 16 December 2002; published 7 August 2003.

Citation: Reid, J. S., et al. (2003), Analysis of measurements of Saharan dust by airborne and ground-based remote sensing methods during the Puerto Rico Dust Experiment (PRIDE), J. Geophys. Res., 108(D19), 8586, doi:10.1029/2002JD002493.

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