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M. Jacox | Climate Variability and the 3D Structure of Coastal Upwelling | October 23, 2014 Climate Variability and the 3D Structure of Coastal Upwelling Michael Jacox October 23, 2014 Collaborators: Andy Moore, Chris Edwards, Jerome Fiechter
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Page 1: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

Climate Variability and the 3D Structure of Coastal Upwelling

Michael JacoxOctober  23,  2014

Collaborators: Andy Moore, Chris Edwards, Jerome Fiechter

Page 2: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Decadal  Scale  Upwelling  Variability  in  the  California  Current  System                                                |                                            July  14,  2014

How Do We Study Upwelling?

Page 3: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

 1800  km  !!

Model Configuration (1988-2010)

oceanmodeling.ucsc.edu

Regional  Ocean  Modeling  System  (ROMS)  4DVAR  Data  Assimilation  (SST,  SSH,  In  situ)  

1/10°  horizontal  resolution  42  vertical  levels    ECMWF  fluxes  

CCMP  wind  San Francisco Bay

Cape Mendocino

Cape Blanco

Pt. Conception

Monterey Bay

2000  km  

Page 4: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

An Overview of CCS Upwelling

Vertical  velocity  is  calculated  at  40m  depth  !Long-­‐term  mean  upwelling  extends  approximately  200  km  offshore  

Three  distinct  regions  (Dorman  and  Winant,  1995):  !North  Storm  track,  variable  forcing  !Central  Persistent  equatorward  winds  !South  Sheltered  from  strong  winds  

Cape  Blanco

Cape  Mendocino

Monterey  Bay

Pt.  Conception

Mean  Vertical  Velocity  (m/day)

San  Francisco  Bay

Page 5: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

An Overview of CCS Upwelling

Cape  Blanco

Cape  Mendocino

Monterey  Bay

Pt.  Conception

Mean  Vertical  Velocity  (m/day)

Upwelling  (m2/s)

Mean  Upwelling  Transport

Cape  Blanco

Cape  Mendocino

Monterey  Bay

Pt.  Conception

San  Francisco  Bay

Page 6: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

Discrepancies in Upwelling Estimates

1.  Upwelling  Index  overestimates  Ekman  Transport  !Discrepancy  between  model  wind  and  upwelling  index  wind  (data  issue)

2.  Ekman  Transport  overestimates  upwelling  !Discrepancy  between  wind-­‐driven  transport  and  vertical  transport  (dynamical  issue)  !Caused  by  cross-­‐shore  geostrophic  flow  (Marchesiello  and  Estrade,  2010)

Upwelling  (m2/s)

1

2

Mean  Upwelling  Transport

Page 7: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

Capturing Interannual Variability in 2D

Cape  Mendocino

Monterey  Bay

Cape  Blanco

Point  Conception

Cape  Mendocino

Monterey  Bay

Cape  Blanco

Point  Conception

2008 2010

Page 8: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

Capturing Interannual Variability in 2D

Year

Cape  Blanco

Monterey  Bay

35%  Explained  Variance

42%  Explained  Variance

PC  Amplitu

dePC

 Amplitu

de

EOF1

EOF1

San  Francisco  Bay

Cape  Mendocino

Point  Conception

Jacox  et  al.  (2014)

47  

46  

45  

44  

43  

42  

41

40  

39  

38  

37  

36  

35

-­‐126                        -­‐124                        -­‐122

Page 9: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

Capturing Interannual Variability in 2D

Cape  Mendocino

Monterey  Bay

Year

42%  Explained  Variance

Cape  Blanco

PC  Amplitu

dePC

 Amplitu

de

11%  Explained  Variance

EOF2

EOF1

San  Francisco  Bay

Jacox  et  al.  (2014)

Point  Conception

47  

46  

45  

44  

43  

42  

41

40  

39  

38  

37  

36  

35

-­‐126                        -­‐124                        -­‐122

Page 10: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

The Central CCS Response to PDO/NPGO

Year

r  =  0.62  r  =  0.61

Jacox  et  al.  (2014)

Page 11: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

The Central CCS Response to PDO/NPGO

Year

r  =  0.62  r  =  0.61

PDO+  NPGO-­‐

PDO-­‐  NPGO+

Jacox  et  al.  (2014)

Page 12: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

The Central/Northern CCS Response to PDO/NPGO

Cape  Blanco

Cape  Mendocino

Monterey  Bay

Cape  Blanco

Cape  Mendocino

Monterey  Bay

PDO+/NPGO-­‐  (1993-­‐1996) PDO-­‐/NPGO+  (2007-­‐2010)

Vertical  Velocity

 Ano

maly  (m

/day)

Vertical  Velocity

 Ano

maly  (m

/day)

San  Francisco  Bay

San  Francisco  Bay

Jacox  et  al.  (2014)

Page 13: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

The Central/Northern CCS Response to PDO/NPGO

Cape  Blanco

Cape  Mendocino

Monterey  Bay

Cape  Blanco

Cape  Mendocino

Monterey  Bay

PDO+/NPGO-­‐  (1993-­‐1996) PDO-­‐/NPGO+  (2007-­‐2010)

Vertical  Velocity

 Ano

maly  (m

/day)

Vertical  Velocity

 Ano

maly  (m

/day)

+25%-­‐71%

+23%

-­‐24%

-­‐17%+25%

-­‐45%

+34%San  Francisco  

BaySan  Francisco  

Bay

Jacox  et  al.  (2014)

Page 14: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

Upwelling Response to Coastal Wind Profiles

Jacox  and  Edwards  (2012)

1988-­‐2010

Distance  From  Coast  (km)

Depth  (m

)

Distance  From  Coast  (km)

Depth  (m

)

PDO+  NPGO-­‐

PDO-­‐  NPGO+

Page 15: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

A Hypothesis on Biological Implications

1993-­‐1996  (PDO+,  NPGO-­‐)

2007-­‐2010  (PDO-­‐,  NPGO+)

Small  Phytoplankton

 Chl  (m

g/m

2 )Large  Ph

ytop

lankton  Ch

l  (mg/m

2 )

NEMURO  biogeochemical  model  coupled  to  ROMS:  !!Two  phytoplankton:    Small  (nanophytoplankton)  Large  (diatoms)

Page 16: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

A Hypothesis on Biological Implications

1993-­‐1996  (PDO+,  NPGO-­‐)

2007-­‐2010  (PDO-­‐,  NPGO+)

Small  Phytoplankton

 Chl  (m

g/m

2 )Large  Ph

ytop

lankton  Ch

l  (mg/m

2 )

NEMURO  biogeochemical  model  coupled  to  ROMS:  !!Two  phytoplankton:    Small  (nanophytoplankton)  Large  (diatoms)

Hypothesis:    Intense  nearshore  upwelling  (PDO-­‐,  NPGO+)  favors  large  phytoplankton  !Widespread  weak  upwelling  (PDO+,  NPGO-­‐)  favors  small  phytoplankton.    !(Rykaczewski  and  Checkley,  2008)

Page 17: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

A Hypothesis on Biological Implications

1993-­‐1996  (PDO+,  NPGO-­‐)

2007-­‐2010  (PDO-­‐,  NPGO+) Difference

Small  Phytoplankton

 Chl  (m

g/m

2 )Large  Ph

ytop

lankton  Ch

l  (mg/m

2 )

Page 18: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

A Hypothesis on Biological Implications

-PDO

Small phytoplankton chlLarge phytoplankton chl

r = 0.62

r = -0.72r = 0.80

Upwelling PC1

Upwelling PC1

1990 1995 2000 2005 2010

1990 1995 2000 2005 2010

Page 19: Climate Variability and the 3D Structure of Coastal Upwelling€¦ · M.Jacox|ClimateVariabilityandthe3DStructureofCoastalUpwelling|October23 ,2014 A Hypothesis on Biological Implications

M.  Jacox                                            |                                              Climate  Variability  and  the  3D  Structure  of  Coastal  Upwelling                                                |                                            October  23,  2014

Sardines and Anchovies: A Physical Mechanism?

Chavez  et  al.  (2003)

Rykaczewski  and  Checkley  (2008)

PDO+  !Widespread  weak  upwelling  !Sardines

PDO+  =  Sardines,  PDO-­‐  =  Anchovies

Weak  upwelling  =  Sardines,  Strong  upwelling  =  Anchovies

PDO-­‐  !Intense  coastal  upwelling  !Anchovies


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