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Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent

Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent

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Page 1: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent

Chlorophyll Based Shortwave Absorption in

POP

Bruce Briegleb

Bill Large

Steve Yeager

Gokhan Danabasoglu

Keith Lindsay

Peter Gent

Page 2: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent

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)

Page 3: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent
Page 4: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent

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

Page 5: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent
Page 6: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent
Page 7: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent

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

Page 8: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent

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

Page 9: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent

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

Page 10: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent
Page 11: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent
Page 12: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent
Page 13: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent
Page 14: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent
Page 15: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent
Page 16: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent
Page 17: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent
Page 18: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent
Page 19: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent
Page 20: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent

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

Page 21: Chlorophyll Based Shortwave Absorption in POP Bruce Briegleb Bill Large Steve Yeager Gokhan Danabasoglu Keith Lindsay Peter Gent

Future Work

• Combine with Gokhan’s mods

• Run coupled test (with, without Gokhan’s?)

• Implement for IPCC?