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FORest Canopy Atmosphere Transfer (FORCAsT) 2.0: model updates and evaluation with observations at a mixed forest site

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 p...

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Published in:Geoscientific Model Development 2021-10, Vol.14 (10), p.6309-6329
Main Authors: Wei, Dandan, Alwe, Hariprasad D, Millet, Dylan B, Bottorff, Brandon, Lew, Michelle, Stevens, Philip S, Shutter, Joshua D, Cox, Joshua L, Keutsch, Frank N, Shi, Qianwen, Kavassalis, Sarah C, Murphy, Jennifer G, Vasquez, Krystal T, Allen, Hannah M, Praske, Eric, Crounse, John D, Wennberg, Paul O, Shepson, Paul B, Bui, Alexander A. T, Wallace, Henry W, Griffin, Robert J, May, Nathaniel W, Connor, Megan, Slade, Jonathan H, Pratt, Kerri A, Wood, Ezra C, Rollings, Mathew, Deming, Benjamin L, Anderson, Daniel C, Steiner, Allison L
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cited_by cdi_FETCH-LOGICAL-c480t-99294717d1003197c1b015fe41eea20e5d90bec46cfa78fb8d39d4add61688543
cites cdi_FETCH-LOGICAL-c480t-99294717d1003197c1b015fe41eea20e5d90bec46cfa78fb8d39d4add61688543
container_end_page 6329
container_issue 10
container_start_page 6309
container_title Geoscientific Model Development
container_volume 14
creator Wei, Dandan
Alwe, Hariprasad D
Millet, Dylan B
Bottorff, Brandon
Lew, Michelle
Stevens, Philip S
Shutter, Joshua D
Cox, Joshua L
Keutsch, Frank N
Shi, Qianwen
Kavassalis, Sarah C
Murphy, Jennifer G
Vasquez, Krystal T
Allen, Hannah M
Praske, Eric
Crounse, John D
Wennberg, Paul O
Shepson, Paul B
Bui, Alexander A. T
Wallace, Henry W
Griffin, Robert J
May, Nathaniel W
Connor, Megan
Slade, Jonathan H
Pratt, Kerri A
Wood, Ezra C
Rollings, Mathew
Deming, Benjamin L
Anderson, Daniel C
Steiner, Allison L
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.
doi_str_mv 10.5194/gmd-14-6309-2021
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T ; Wallace, Henry W ; Griffin, Robert J ; May, Nathaniel W ; Connor, Megan ; Slade, Jonathan H ; Pratt, Kerri A ; Wood, Ezra C ; Rollings, Mathew ; Deming, Benjamin L ; Anderson, Daniel C ; Steiner, Allison L</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c480t-99294717d1003197c1b015fe41eea20e5d90bec46cfa78fb8d39d4add61688543</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Aerosols</topic><topic>Air temperature</topic><topic>Atmosphere</topic><topic>Atmospheric boundary layer</topic><topic>Atmospheric chemistry</topic><topic>Boundary layers</topic><topic>Canopies</topic><topic>Canopy</topic><topic>Chemical reactions</topic><topic>Chemistry</topic><topic>Deposition</topic><topic>Dry deposition</topic><topic>Eddy diffusion</topic><topic>Eddy diffusivity</topic><topic>Forests</topic><topic>Gases</topic><topic>Isoprene</topic><topic>Ketones</topic><topic>Modules</topic><topic>Nitrates</topic><topic>Organic nitrates</topic><topic>Oxidation</topic><topic>Parameterization</topic><topic>Plant cover</topic><topic>Secondary aerosols</topic><topic>Splitting</topic><topic>Vertical mixing</topic><topic>VOCs</topic><topic>Volatile organic compounds</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wei, Dandan</creatorcontrib><creatorcontrib>Alwe, Hariprasad D</creatorcontrib><creatorcontrib>Millet, Dylan B</creatorcontrib><creatorcontrib>Bottorff, Brandon</creatorcontrib><creatorcontrib>Lew, Michelle</creatorcontrib><creatorcontrib>Stevens, Philip S</creatorcontrib><creatorcontrib>Shutter, Joshua D</creatorcontrib><creatorcontrib>Cox, Joshua L</creatorcontrib><creatorcontrib>Keutsch, Frank N</creatorcontrib><creatorcontrib>Shi, Qianwen</creatorcontrib><creatorcontrib>Kavassalis, Sarah C</creatorcontrib><creatorcontrib>Murphy, Jennifer G</creatorcontrib><creatorcontrib>Vasquez, Krystal T</creatorcontrib><creatorcontrib>Allen, Hannah M</creatorcontrib><creatorcontrib>Praske, Eric</creatorcontrib><creatorcontrib>Crounse, John D</creatorcontrib><creatorcontrib>Wennberg, Paul O</creatorcontrib><creatorcontrib>Shepson, Paul B</creatorcontrib><creatorcontrib>Bui, Alexander A. 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T</au><au>Wallace, Henry W</au><au>Griffin, Robert J</au><au>May, Nathaniel W</au><au>Connor, Megan</au><au>Slade, Jonathan H</au><au>Pratt, Kerri A</au><au>Wood, Ezra C</au><au>Rollings, Mathew</au><au>Deming, Benjamin L</au><au>Anderson, Daniel C</au><au>Steiner, Allison L</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>FORest Canopy Atmosphere Transfer (FORCAsT) 2.0: model updates and evaluation with observations at a mixed forest site</atitle><jtitle>Geoscientific Model Development</jtitle><date>2021-10-21</date><risdate>2021</risdate><volume>14</volume><issue>10</issue><spage>6309</spage><epage>6329</epage><pages>6309-6329</pages><issn>1991-9603</issn><issn>1991-959X</issn><issn>1991-962X</issn><eissn>1991-9603</eissn><eissn>1991-962X</eissn><abstract>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 &gt;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.</abstract><cop>Katlenburg-Lindau</cop><pub>Copernicus GmbH</pub><doi>10.5194/gmd-14-6309-2021</doi><tpages>21</tpages><orcidid>https://orcid.org/0000-0001-8291-8242</orcidid><orcidid>https://orcid.org/0000-0003-4707-2290</orcidid><orcidid>https://orcid.org/0000-0003-4540-4212</orcidid><orcidid>https://orcid.org/0000-0003-3076-125X</orcidid><orcidid>https://orcid.org/0000-0002-9533-215X</orcidid><orcidid>https://orcid.org/0000-0003-3690-0046</orcidid><orcidid>https://orcid.org/0000-0002-9826-9811</orcidid><orcidid>https://orcid.org/0000-0002-6126-3854</orcidid><orcidid>https://orcid.org/0000-0001-9899-4215</orcidid><orcidid>https://orcid.org/0000-0001-8865-5463</orcidid><orcidid>https://orcid.org/0000-0002-1205-1564</orcidid><orcidid>https://orcid.org/0000-0001-5443-729X</orcidid><orcidid>https://orcid.org/0000-0002-5597-6233</orcidid><oa>free_for_read</oa></addata></record>
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identifier ISSN: 1991-9603
ispartof Geoscientific Model Development, 2021-10, Vol.14 (10), p.6309-6329
issn 1991-9603
1991-959X
1991-962X
1991-9603
1991-962X
language eng
recordid cdi_proquest_journals_2583768795
source Publicly Available Content (ProQuest)
subjects Aerosols
Air temperature
Atmosphere
Atmospheric boundary layer
Atmospheric chemistry
Boundary layers
Canopies
Canopy
Chemical reactions
Chemistry
Deposition
Dry deposition
Eddy diffusion
Eddy diffusivity
Forests
Gases
Isoprene
Ketones
Modules
Nitrates
Organic nitrates
Oxidation
Parameterization
Plant cover
Secondary aerosols
Splitting
Vertical mixing
VOCs
Volatile organic compounds
title FORest Canopy Atmosphere Transfer (FORCAsT) 2.0: model updates and evaluation with observations at a mixed forest site
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