An Automated Common Algorithm for Planetary Boundary Layer Retrievals Using Aerosol Lidars in Support of the U.S. EPA Photochemical Assessment Monitoring Stations Program

Author:

Caicedo Vanessa12,Delgado Ruben12,Sakai Ricardo3,Knepp Travis45,Williams David6,Cavender Kevin7,Lefer Barry8,Szykman James56

Affiliation:

1. a Joint Center of Earth Systems Technology, Baltimore, Maryland

2. b University of Maryland, Baltimore County, Baltimore, Maryland

3. c Howard University, Washington, D.C.

4. d Science Systems and Applications, Inc., Hampton, Virginia

5. e National Aeronautics and Space Administration Langley Research Center, Hampton, Virginia

6. f Office of Research and Development, U.S. Environmental Protection Agency, Research Triangle Park, North Carolina

7. g Office of Air Quality Planning and Standards, U.S. Environmental Protection Agency, Research Triangle Park, North Carolina

8. h National Aeronautics and Space Administration Headquarters, Washington, D.C.

Abstract

AbstractA unique automated planetary boundary layer (PBL) retrieval algorithm is proposed as a common cross-platform method for use with commercially available ceilometers for implementation under the redesigned U.S. Environmental Protection Agency Photochemical Assessment Monitoring Stations program. This algorithm addresses instrument signal quality and screens for precipitation and cloud layers before the implementation of the retrieval method using the Haar wavelet covariance transform. Layer attribution for the PBL height is supported with the use of continuation and time-tracking parameters, and uncertainties are calculated for individual PBL height retrievals. Commercial ceilometer retrievals are tested against radiosonde PBL height and cloud-base height during morning and late-afternoon transition times, critical to air quality model prediction and when retrieval algorithms struggle to identify PBL heights. A total of 58 radiosonde profiles were used, and retrievals for nocturnal stable layers, residual layers, and mixing layers were assessed. Overall good agreement was found for all comparisons, with one system showing limitations for the cases of nighttime surface stable layers and daytime mixing layer. It is recommended that nighttime shallow stable-layer retrievals be performed with a recommended minimum height or with additional verification. Retrievals of residual-layer heights and mixing-layer comparisons revealed overall good correlations with radiosonde heights (square of correlation coefficientsr2ranging from 0.89 to 0.96, and bias ranging from approximately −131 to +63 m for the residual layer andr2from 0.88 to 0.97 and bias from −119 to +101 m for the mixing layer).

Funder

Goddard Space Flight Center

National Oceanic and Atmospheric Administration

Publisher

American Meteorological Society

Subject

Atmospheric Science,Ocean Engineering

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