usgs r/v polaris retires: we reflect on what she taught us · usgs r/v polaris retires: we reflect...

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USGS R/V Polaris Retires: We reflect on what she taught us Erica Nejad, Charles Martin, Tara Schraga, Jim Cloern US Geological Suvey Five decades and 1100 research cruises aboard the R/V Polaris have documented a remarkable range of San Francisco Bay condi;ons Jan Apr Aug 9 10 11 12 12 14 16 18 18 20 22 0 10 20 30 0 10 20 30 0 10 20 30 Salinity Temperature (° C) 19692013 20142015 Record high water temperatures in 2014-15, years of the warm blob Mean January, April and August temperature along the salinity gradient for two eras: 1969-2013 and 2014-2015 Lowest during El Niño year floods and highest during prolonged droughts Monthly monitoring includes measurements of : Salinity Temperature Dissolved Oxygen Chlorophyll-a Nutrients Suspended Par;culate maVer Light Penetra;on Phytoplankton Composi;on Phytoplankton Toxins What extreme highs and lows have we recorded over this period and what are the physical and ecological circumstances surrounding them? WATER TEMPERATURE &CLIMATE ANOMALIES SALINITY IN SOUTH BAY TIED TO DELTA OUTFLOW FRESH WATER AT THE GOLDEN GATE SUPERSATURATED OXYGEN Lower South Bay South Bay Central Bay Large phytoplankton bloom in South Bay (up to 480ug/L) Super saturated DO up to 140% extending from Lower South Bay to almost Central Bay. (long term average = 90%) March 1998 oxygen super satura;on event caused by a huge bloom of diatoms in the South Bay. 1965 1970 1975 1980 1990 1995 2000 2005 2010 2015 0 5 10 15 20 25 30 35 Salinity HIGHEST CHL-A,SACRAMENTO RIVER 1975 1980 1990 1995 2000 2005 2010 2015 0 10 20 30 40 50 60 70 Calculated Chlorophyll (ug/L) 10 30 50 70 Yolo Bypass Dry Yolo Bypass Flooded Largest phytoplankton bloom detected in Sacramento river sta;ons was May 2016, likely produced in the Yolo Bypass when it was flooded by a large El Niño storm Sta;on 25-30 surface salinity and yearly averaged delta oublow from hVp://www.water.ca.gov/dayflow/ Near freshwater at the surface of Sta;on 18 during the February 1998 El Niño flood In service from : 1969-2015 Long term research allows us to view extremes in the context of a historic baseline All examples of extreme events highlight the bay responding to climate events CONCLUSIONS sday.wr.usgs.gov/access/wqdata/index.html Contact: Erica Nejad ([email protected]) Photos: hVp://earthobservatory.nasa.gov/IOTD/view.php?id=87719 + PROLONGED DROUGHT (1987-92) DROUGHT (2007-09) EL NIÑO (1982-83) EXTREME DROUGHT (1976-77) DROUGHT (2014-15) EL NIÑO (1997-98)

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Page 1: USGS R/V Polaris Retires: We reflect on what she taught us · USGS R/V Polaris Retires: We reflect on what she taught us Erica Nejad, Charles Martin, Tara Schraga, Jim Cloern US Geological

USGS R/V Polaris Retires: We reflect on what she taught us

USGS R/V Polaris Retires: We reflect on what she taught us

Erica Nejad, Charles Martin, Tara Schraga, Jim CloernUS Geological Suvey

Fivedecadesand1100researchcruisesaboardtheR/VPolarishavedocumentedaremarkablerangeof

SanFranciscoBaycondi;onsJan Apr Aug

9

10

11

12

12

14

16

18

18

20

22

0 10 20 30 0 10 20 30 0 10 20 30Salinity

Tem

pera

ture

(° C

)

1969−2013

2014−2015

Recordhighwatertemperaturesin2014-15,yearsofthewarmblob

MeanJanuary,AprilandAugusttemperaturealongthesalinitygradientfortwoeras:1969-2013and2014-2015

LowestduringElNiñoyearfloodsandhighestduringprolongeddroughts

Monthlymonitoringincludesmeasurementsof:•  Salinity•  Temperature•  DissolvedOxygen•  Chlorophyll-a•  Nutrients•  SuspendedPar;culatemaVer•  LightPenetra;on•  PhytoplanktonComposi;on•  PhytoplanktonToxins

What extreme highs and lows have we

recorded over this period and what are

the physical and ecological

circumstances surrounding them?

WATERTEMPERATURE&CLIMATEANOMALIES

SALINITYINSOUTHBAYTIEDTODELTAOUTFLOW

FRESHWATERATTHEGOLDENGATE

SUPERSATURATEDOXYGEN

Lower South Bay South Bay Central Bay

Large phytoplankton bloom in South Bay (up to 480ug/L)

Super saturated DO up to 140% extending from Lower South Bay

to almost Central Bay. (long term average = 90%)

March1998oxygensupersatura;oneventcausedbyahugebloomofdiatomsintheSouthBay.

1965 1970 1975 1980 1990 1995 2000 2005 2010 20150

5

10

15

20

25

30

35

Salin

ity

HIGHESTCHL-A,SACRAMENTORIVER

1975 1980 1990 1995 2000 2005 2010 2015

0

10

20

30

40

50

60

70

Cal

cula

ted

Chl

orop

hyll

(ug/

L)

10

30

50

70

Yolo Bypass Dry Yolo Bypass Flooded

LargestphytoplanktonbloomdetectedinSacramentoriversta;onswasMay2016,likelyproducedintheYoloBypasswhenitwasfloodedbyalargeElNiñostorm

Sta;on25-30surfacesalinityandyearlyaverageddeltaoublowfromhVp://www.water.ca.gov/dayflow/

NearfreshwateratthesurfaceofSta;on18duringtheFebruary1998ElNiñoflood

Inservicefrom:1969-2015

•  Longtermresearchallowsustoviewextremesinthecontextofahistoricbaseline•  Allexamplesofextremeeventshighlightthebayrespondingtoclimateevents

CONCLUSIONS

Lower South Bay South Bay Central Bay

sday.wr.usgs.gov/access/wqdata/index.htmlContact:EricaNejad([email protected])

Photos:hVp://earthobservatory.nasa.gov/IOTD/view.php?id=87719

+

PROLONGEDDROUGHT(1987-92)

DROUGHT(2007-09)

ELNIÑO(1982-83)

EXTREMEDROUGHT(1976-77)

DROUGHT(2014-15)

ELNIÑO(1997-98)