Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan...
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![Page 1: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent.](https://reader033.fdocuments.us/reader033/viewer/2022042821/56649ca45503460f949650fa/html5/thumbnails/1.jpg)
Chlorophyll Based Shortwave Absorption in
POP
Bruce Briegleb
Bill Large
Steve Yeager
Gokhan Danabasoglu
Keith Lindsay
Peter Gent
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Chlorophyll Based Absorption
Why?
• Present absorption based on Jerlov water type IA Constant in space and time
• Vertical distribution of shortwave absorption important to ocean modeling (as shown in 1D boundary layer models)
• Chlorophyll data available (we used SeaWIFS over September 1997 to November 2001)
• Transmission parameterization available (Carter Ohlmann’s chlorophyll-dependent)
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Chlorophyll Transmission from Carter Ohlmann
• A_1 exp(-B_1 z) + A_2 exp(-B_2 z)• A,B chlorophyll dependent: range of chl from .001
mg/m^3 to 10 mg/m^3• A,B from empirical fits to atmosphere-ocean radiative
transfer calculations• Solar zenith angle and cloud effects ignored• Overall precision of transmission about .005• Transmission compared well to EPIC and TOGA-
COARE observations
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Implementation
• Controlled by namelist input. Default transmission available, as well as top layer
• Monthly climatology of chlorophyll data• Chlorophyll assumed uniformly mixed
vertically through column• Chlorophyll based transmission computed
once a month and stored in a look-up table• New sw_absorb.F module
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Testing
• Control from Keith Lindsay
• Ocean only
• gx3 with1991-1993 NCEP/ISCCP forcing
• 350 years accelerated; 50 years synchronous
• Chlorophyll absorption run from year 400 to 423. Years 421-423 compared to control
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Absorbed Shortwave Fluxes (W/m^2)Global Mean Ocean Year 400
Chlorophyll Jerlov IA Diff
Total 172.3 172.3 0.0
Top Layer 132.2 144.2 -12.0
Bnd Layer minus top
12.4 6.9 +5.5
Deep below bnd layer
27.7 21.2 +6.5
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Test Results: Ocean Only
• SST cools in subtropics about .1C to .2C• SST warms along equator about 0.5C,
coasts 1C• Only small changes in SST seasonal cycle• Tropical and sub-tropical waters between
~40m and ~200m depth warm about 0.5C• Significant response in Pacific Equatorial
Undercurrent
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Future Work
• Combine with Gokhan’s mods
• Run coupled test (with, without Gokhan’s?)
• Implement for IPCC?