Deon Louw presentation - Benguela Current Commission
Transcription
Deon Louw presentation - Benguela Current Commission
Detecting phytoplankton dynamics in the central Benguela current upwelling ecosystem off Namibia by using in situ chlorophyll-α measurements. • • • Ministry of Fisheries and Marine Resources & Leibniz Institute for Baltic Sea Research Warnemünde D.C. Louw Anja Eggert Anja van der Plas Volker Mohrholz Objectives • Longterm variability of chlorophyll [ ] • Quantifying phytoplankton blooms • Seasonality of phytoplankton blooms/peaks Methods/Data 0 Depth (db) -100 -200 -300 70 60 50 40 30 Distance offshore (nm) 20 10 0 Month 2001 2002 2003 2004 2005 2006 2007 2008 2009 2010 2011 2012 2 30-Jan-01 2-Feb-02 1-Feb-03 27-Jan-04 11-Feb-05 28-Jan-10 3 1-Mar-01 28-Feb-02 4-Mar-03 8-Mar-05 3-Mar-06 6-Mar-08 25-Feb-09 10-Mar-10 14-Mar-11 4 3-Apr-01 No Data 15-Apr-03 28-Mar-04 28-Mar-06 13-Apr-08 1-Apr-09 8-Apr-10 12-Apr-11 16-Mar-12 5 1-May-01 29-Apr-02 13-May-03 12-May-04 12-May-05 7-May-07 28-Apr-09 No Data 6 4-Jun-01 4-Jun-02 12-Jun-03 1-Jun-04 30-May-06 28-May-08 26-May-10 17-May-11 7 3-Jul-01 9-Jul-02 1-Jul-03 29-Jun-04 30-Jun-05 4-Jul-06 10-Jul-07 1-Jul-08 29-Jun-09 12-Jul-10 7-Jul-11 8 31-Jul-01 4-Aug-02 8-Aug-03 5-Aug-04 31-Jul-08 9 5-Sep-01 3-Sep-02 4-Sep-03 31-Aug-04 2-Sep-05 28-Aug-06 3-Sep-07 5-Sep-08 20-Aug-09 8-Sep-11 4-Sep-12 10 2-Oct-01 1-Oct-02 1-Oct-03 29-Sep-04 13-Oct-08 16-Sep-09 9-Oct-12 11 6-Nov-01 29-Oct-02 4-Nov-03 2-Nov-04 8-Nov-05 1-Nov-06 6-Nov-07 30-Oct-09 27-Oct-10 6-Nov-12 12 4-Dec-01 5-Dec-02 10-Dec-03 30-Nov-04 2-Dec-05 6-Dec-07 6-Dec-08 1-Dec-09 2-Dec-10 Not Data 29-Nov-12 Temperature (15m & 10nm station) 70nm (15m) 40nm 10nm Jul99 10nm Station Jul00 Jul01 Jul02 Jul03 Jul04 Jul05 Jul06 Jul07 Jul08 Jul09 Jul10 Jul11 Jul12 Temperature (Seasonality) Summer • Stratified • >16°C • Strong thermocline Nutrients Upwelling • Mixed • < 13°C Autum/Winter • Mixed • 13°-16°C Nutrients Summer • Stratified • Weak Thermocline Nu tri en ts Chlorophyll (Stations) Variability high Decrease in chlorophll offshore direction 2nm station not as high as expected (mixing/turbulents/waves) 5-20nm stations simallar biomass (highest production) 30-70nm stations (lowest production) 0 10 20 30 -1 Chl a [µg L ] 40 50 • • • • • 70nm 60nm 50nm 40nm 30nm 20nm 10nm 5nm 2nm Longterm trend/variability 0 200 400 -2 Chl a [mg m ] 600 • Interannual variability high • not a significant trend 2001 01/02 02/03 03/04 04/05 05/06 06/07 07/08 08/09 09/10 10/11 11/12 2012 Phytoplankton Blooms (surface) Raw Readings Major Blooms Minor Blooms 18.4 µg/L 12.9µg/L Define Blooms Constant threshold value • Mean (12years) + 2SD´s, = MajBl • MinBl= Remove MajBl & recalculate as above Constant threshold = understanding the long term changes in biomass (Kim et al, 2009) Phytoplankton Blooms (surface) Raw Readings Major Blooms Minor Blooms 18.4 µg/L 12.9µg/L Constant threshold = understanding the long term changes in biomass Defined Blooms Constant threshold value • Mean + 2SD´s, above the long term mean (12years) = MajBl • MinBl= Remove MajBl & recalculate as above (Kim et al, 2009) Climatology of Chl [ ] Median Major Blooms Minor Blooms 9.96 µg/L 8.12 µg/L LATE SUMMER PEAKS • Larger bloom • Spread over larger area • Major peak is sub-surface SPRING PEAKS • Sub-surface • Spread almost homogenically EARLY SUMMER PEAKS • Closer to the surface • January ???? Peaks • April/May (summer/Autum) • August (Spring Bloom) • December (Beginning summer) 800 0 200 400 -2 -2 Chl a [mg m ] 600 April/May April/May August/September August/September December December 2001 01/02 02/03 03/04 04/05 05/06 06/07 07/08 08/09 09/10 10/11 11/12 2012 Summary • Inshore stations showed significant similarities • High Chl [ ] inner shelf • Low Chl [ ] offshore • Variability of Chl is high Blooms Not high frequency of major blooms as well as minor blooms (missing data) Initiation of blooms does not end up in a Minor Bloom or Major Bloom Seasonality April/May Peak (Late summer) • Not a direct consequence of upwelling but rather the breakdown of the thermocline due to cooling of the atmospheric system • Largest blooms • Largest contributor to annual biomass • Sub-surface blooms August Peak (Upwelling) • Directly due to upwelling • Biomass lower • Mixing high • Sub-surface Chl maxima (minor bloom) December Peak (Early Summer) • Closer to the surface
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