Skip navigation and jump second-level navigation.Skip navigation and jump to main content of the page.
 Home | Site Map | Glossary | FAQs | LibraryInside NWFSC

  
 

NOAA logo: go to NOAA web site

NWFSC home
NMFS home


salmon
 


   
    
   Home   Research   Publications   Resources   Events   Education   Contact Us  
         Divisions     Programs/Projects/Teams     Collaborative Projects     Staff Profiles     Facilities      Vessels     
            
Phytoplankton Biomass



Home

 •September 2008 Update
 •Forecast of Adult Returns
 •Adult Return Data

Large–scale Ocean and Atmospheric Indicators

 •Pacific Decadal Oscillation (PDO)
 •Multivariate El Niño Southern Oscillation Index (MEI)
 • Basin-scale winds

Local and Regional Physical Indicators

 •Sea surface temperature anomalies
 •Coastal upwelling
 •Physical spring transition
 •Deep–water temperature and salinity

Local Biological Indicators

 •Copepod biodiversity
 •Northern copepod anomalies
 •Copepod community structure
 •Biological spring transition
 •June spring Chinook
 •September coho
 •Zooplankton species composition

Indicators Under Development

 •A second mode of North Pacific sea surface temperature variation
 •Phytoplankton biomass
 •Euphausiid egg concentration, adult biomass, and production rates
 •Interannual variation in habitat area
 •Forage fish and Pacific hake abundance
 •Salmon predation index
 •Potential indices for future development

Introduction to Pacific Northwest Oceanography

 •Physical oceanographic considerations
 • Climate–scale physical variability

Ocean Sampling Methods

 •Hydrography, zooplankton, and ichthyoplankton
 •Juvenile salmon sampling

Acknowledgements

References

Archive of Updates and Forecasts

Links

Glossary

 

Phytoplankton Biomass


Based on samples collected along the Newport Hydrographic Line, we developed time series of both total chlorophyll and the fraction of chlorophyll smaller than 10 µm.  These data serve as estimates of phytoplankton biomass, and both data types will be used to describe interannual variation in timing of the spring bloom (which can occur between February and April), as well as blooms in summer during July–August upwelling.  These measures should provide an index of potential conditions (good vs. poor) for spawning of copepods and euphausiids. 





last modified 03/11/2008

              
   
Inside NWFSC       NOAA       NMFS       OHH       Library       CB       FE       EC       FRAM       REUT       OMI       SD
Home     About Us     Site Map     Privacy Policy     Copyright Policy     Disclaimer     Accessibility     Feedback Form