FORest Canopy Atmosphere Transfer (FORCAsT) 2.0: model updates and evaluation with observations at a mixed forest site
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2021
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Journal Title:Geoscientific Model Development
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Personal Author:Wei, Dandan
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Alwe, Hariprasad D.
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Millet, Dylan B.
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Bottorff, Brandon
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Lew, Michelle
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Stevens, Philip S.
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Shutter, Joshua D.
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Cox, Joshua L.
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Keutsch, Frank N.
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Shi, Qianwen
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Kavassalis, Sarah C.
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Murphy, Jennifer G.
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Vasquez, Krystal T.
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Allen, Hannah M.
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Praske, Eric
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Crounse, John D.
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Wennberg, Paul O.
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Shepson, Paul B.
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Bui, Alexander A. T.
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Wallace, Henry W.
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Griffin, Robert J.
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May, Nathaniel W.
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Connor, Megan
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Slade, Jonathan H.
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Pratt, Kerri A.
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Wood, Ezra C.
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Rollings, Mathew
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Deming, Benjamin L.
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Anderson, Daniel C.
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Steiner, Allison L.
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NOAA Program & Office:
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Description:The FORCAsT (FORest Canopy Atmosphere Transfer) model version 1.0 is updated to FORCAsT 2.0 by implementing five major changes, including (1) a change to the operator splitting, separating chemistry from emission and dry deposition, which reduces the run time of the gas-phase chemistry by 70 % and produces a more realistic in-canopy profile for isoprene; (2) a modification of the eddy diffusivity parameterization to produce greater and more realistic vertical mixing in the boundary layer, which ameliorates the unrealistic simulated end-of-day peaks in isoprene under well-mixed conditions and improves daytime air temperature; (3) updates to dry deposition velocities with available measurements; (4) implementation of the Reduced Caltech Isoprene Mechanism (RCIM) to reflect the current knowledge of isoprene oxidation; and (5) extension of the aerosol module to include isoprene-derived secondary organic aerosol (iSOA) formation. Along with the operator splitting, modified vertical mixing, and dry deposition, RCIM improves the estimation of first-generation isoprene oxidation products (methyl vinyl ketone and methacrolein) and some second-generation products (such as isoprene epoxydiols). Inclusion of isoprene in the aerosol module in FORCAsT 2.0 leads to a 7 % mass yield of iSOA. The most important iSOA precursors are IEPOX and tetrafunctionals, which together account for >86 % of total iSOA. The iSOA formed from organic nitrates is more important in the canopy, accounting for 11 % of the total iSOA. The tetrafunctionals compose up to 23 % of the total iSOA formation, highlighting the importance of the fate (i.e., dry deposition and gas-phase chemistry) of later-generation isoprene oxidation products in estimating iSOA formation.
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Source:Geoscientific Model Development, 14(10), 6309-6329
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ISSN:1991-9603
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Rights Information:CC BY
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Compliance:Library
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Main Document Checksum:urn:sha256:aa99f29ef4b9402b375c79a52d8a0b2d118552725ffcaa6dcbb2d791fc02e732
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