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A comparison of scavenging and deposition processes in global models: Results from the WCRP Cambridge workshop of 1995

  • P. J. Rasch
  • , J. Feichter
  • , K. Law
  • , N. Mahowald
  • , J. Penner
  • , C. Benkovitz
  • , C. Genthon
  • , C. Giannakopoulos
  • , P. Kasibhatla
  • , D. Koch
  • , H. Levy
  • , T. Maki
  • , M. Prather
  • , D. L. Roberts
  • , G. J. Roelofs
  • , D. Stevenson
  • , Z. Stockwell
  • , S. Taguchi
  • , M. Kritz
  • , M. Chipperfield
  • D. Baldocchi, P. McMurry, L. Barrie, Y. Balkanski, R. Chatfield, E. Kjellstrom, M. Lawrence, H. N. Lee, J. Lelieveld, K. J. Noone, J. Seinfeld, G. Stenchikov, S. Schwartz, C. Walcek, D. Williamson
  • National Center for Atmospheric Research
  • Max Planck Institute for Meteorology
  • University of Cambridge
  • University of California, Santa Barbara
  • University of Michigan, Ann Arbor
  • Brookhaven National Laboratory
  • UJF
  • Duke University
  • NASA Goddard Institute for Space Studies
  • GFDL
  • JMA
  • Long Beach VA and University of California
  • Now at Met Office Hadley Centre
  • Universiteit Utrecht
  • NIRE
  • State University of New York Albany
  • ATDD NOAA
  • University of Minnesota Twin Cities
  • AES Downsview Laboratory
  • CEA/UVSQ/CNRS
  • MISU
  • MPI for Chemistry
  • EML USDOE NY
  • University of Maryland, College Park

Research output: Contribution to journalArticlepeer-review

153 Citations (Scopus)

Abstract

We report on results from a World Climate Research Program workshop on representations of scavenging and deposition processes in global transport models of the atmosphere. 15 models were evaluated by comparing simulations of radon, lead, sulfur dioxide, and sulfate against each other, and against observations of these constituents. This paper provides a survey on the simulation differences between models. It identifies circumstances where models are consistent with observations or with each other, and where they differ from observations or with each other. The comparison shows that most models are able to simulate seasonal species concentrations near the surface over continental sites to within a factor of 2 over many regions of the globe. Models tend to agree more closely over source (continental) regions than for remote (polar and oceanic) regions. Model simulations differ most strongly in the upper troposphere for species undergoing wet scavenging processes. There are not a sufficient number of observations to characterize the climatology (long-term average) of species undergoing wet scavenging in the upper troposphere. This highlights the need for either a different strategy for model evaluation (e.g., comparisons on an event by event basis) or many more observations of a few carefully chosen constituents.

Original languageEnglish
Pages (from-to)1025-1056
Number of pages32
JournalTellus, Series B: Chemical and Physical Meteorology
Volume52
Issue number4
DOIs
Publication statusPublished - 1 Jan 2000
Externally publishedYes

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

  1. SDG 13 - Climate Action
    SDG 13 Climate Action

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