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Primary production in the Arctic Ocean: Future changes in physics ...

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<strong>Primary</strong><strong>production</strong><strong>in</strong><strong>the</strong><strong>Arctic</strong><br />

<strong>Ocean</strong>:<strong>Future</strong><strong>changes</strong><strong>in</strong><strong>physics</strong>,<br />

nutrients,andcarbon<br />

PatriciaMatrai<br />

(withalittlehelpfrommyfriends)<br />

BigelowLaboratoryfor<strong>Ocean</strong>Sciences


Foto:NationalGeographic


Photo: MikeBritta<strong>in</strong>


SwissGlobalChangeDay2013Bern<br />

Whatare<strong>the</strong>se<br />

(charismaticmegafauna)<br />

resourcesbasedupon?


Charismatic microflora!<br />

Plant (phyto) plankton: Different diatoms<br />

(hundred micrometres <strong>in</strong> size, sta<strong>in</strong>ed)<br />

SwissGlobalChangeDay2013Bern


SwissGlobalChangeDay2013Bern<br />

Phytoplankton


Howcanproductivitybe<strong>in</strong>fluencedbychange?<br />

1. Bottomup effects:<br />

Environmental change affects consumers<br />

by modulat<strong>in</strong>g <strong>the</strong> productivity, tim<strong>in</strong>g<br />

and/or size of primary producers.<br />

2.Topdowneffects:<br />

Alteredpredationbyconsumeraffects<br />

<strong>the</strong>structureand/orproductivityof<br />

lowerfoodweb.<br />

SwissGlobalChangeDay2013Bern (F<strong>in</strong>kel etal.2009,JPlk Res) CourtesyJETremblay


Bottomupchange:lessice=morelight<br />

1.Extent(Septemberm<strong>in</strong>imum) 2.Age(thickness)<br />

Source:NSDIC<br />

SwissGlobalChangeDay2013Bern<br />

Source:NSDIC<br />

3.Seasonalpersistence<br />

ofannualice:2to13<br />

daysperdecade<br />

years<br />


<strong>Primary</strong><strong>production</strong>patternsarenotasimplefunctionoflight<br />

Meanannual<strong>in</strong>cident<br />

<strong>in</strong>solation(20350Wm 2 )<br />

Kallberg etal.(2005).<br />

SwissGlobalChangeDay2013Bern<br />

<strong>Primary</strong>Production<br />

?<br />

Light<br />

Meanannualchlorophyll<br />

(=phytoplanktonbiomass)<br />

NASA<br />

CourtesyJETremblay


Ice melt and surface<br />

warm<strong>in</strong>g result <strong>in</strong><br />

stratification that<br />

prevents vertical<br />

mix<strong>in</strong>g<br />

Low nutrient supply<br />

to surface and thus<br />

low harvestable<br />

productivity<br />

Deepoceanarea<br />

nutrients<br />

sediment<br />

SwissGlobalChangeDay2013Bern CourtesyPWassmann


Howdeep?<br />

Seasonaldistributionofeuphoticzoneandmixed<br />

layerdepthsfromspr<strong>in</strong>gtofall<strong>in</strong><strong>the</strong><strong>Arctic</strong><strong>Ocean</strong><br />

Euphoticzonedepth[m]=>Light<br />

Nodata<br />

100 0<br />

Mixedlayerdepth[m]=>Nutrients<br />

Satellitebasedandfielddata<br />

monthlyaverages(19982007)<br />

April<br />

May<br />

June<br />

July<br />

August<br />

September<br />

SwissGlobalChangeDay2013Bern<br />

Hill,Matrai etal.2013


Today sextreme<br />

Sameamount<br />

Sameamount seasonal<br />

ofnutrients ofnutrients variation<br />

disappears<br />

Same Same<br />

harvestable<br />

harvestable<br />

<strong>production</strong><br />

SwissGlobalChangeDay2013Bern<br />

Wassmann 2011,andthosebeforehim


Whereis<strong>Arctic</strong><strong>Primary</strong>Productionnow?


IntegratedAnnualNet<strong>Primary</strong>Production(PP)<br />

(19542007field;19982007satellitedata)<br />

SwissGlobalChangeDay2013Bern<br />

AlgorithmestimatedNPPbasedon:<br />

FieldChl SatChl<br />

0-100 gC m -2 yr -1<br />

Hill,Matrai etal.2013


NetCommunityProduction<br />

=<br />

NCP*f factor=NPP(orNP?)<br />

(0200)<br />

(040)gC m2 yr1 SwissGlobalChangeDay2013Bern<br />

10<br />

0<br />

30<br />

10<br />

Codispoti ,Matrai etal.2013<br />

5<br />

0


Abiologicalmodelappliedregionally<br />

Panarcticdecadaltrend<br />

Pabi etal.2008<br />

Arrigo andvanDijken 2011<br />

us<strong>in</strong>gsatellitedata<br />

Variableregionaldecadaltrends<br />

H<strong>in</strong>dcast<strong>in</strong>g <strong>in</strong>to<strong>the</strong>1970s


Pan<strong>Arctic</strong>representationof<strong>the</strong>present<br />

MeanannualwatercolumnPP[gC m 2 y 1 ]by5modelsandasatellitederivedestimate<br />

Popova etal.2010 Dealetal.2011 Zhangetal.2010<br />

Dupont etal.2012 Yool etal.2011<br />

SwissGlobalChangeDay2013Bern<br />

field<br />

data?


Realitycheckorvalidation<br />

• Ourprojectionsareonlyasgoodasourdataare:<br />

– Enoughbiologicaldatatovalidate?<br />

• Yearround;arcticwide;undericeandiceedgeblooms<br />

– Appropiate physicalandbiologicalmodels?<br />

• Currentparameterizationsofmixedlayerdepth, nutrient<br />

fields,verticaldistributionofphytoplanktonbiomass<br />

– Factorswithnew orun<strong>in</strong>tendedeffects?<br />

• Clouds,w<strong>in</strong>ds,freshwaterstratification


SwissGlobalChangeDay2013Bern<br />

IntegratedAnnualNPP<br />

ARCSSPP&nutrientsdatasets19542007<br />

(www.nodc.noaa.gov)<br />

Hill,Matrai etal.2013<br />

AlsoseeArdyna etal.2013BGD


Subsurfacechlorophyllmaximum<br />

(=phytoplanktonbiomass):<br />

seasonalandregionalvs.annualandpanarcticscales<br />

Whereare<br />

<strong>the</strong>phytos<br />

and<br />

when?<br />

Depth[m]<br />

0 350days<br />

Chl (mgm 3 )<br />

Ardyna etal.2013BGD<br />

andalso<br />

Hill,Matrai etal.2013<br />

Arrigo,Matrai,vanDijken 2011


Modeledmixedlayerdep<strong>the</strong>xamples<br />

SwissGlobalChangeDay2013Bern<br />

Popova etal.2012<br />

Same<br />

forDIN<br />

fields


Lightdecrease<br />

(820%)<br />

(+clouds)<br />

(19982009)<br />

ABOVEsea<br />

(ice)surface<br />

SwissGlobalChangeDay2013Bern<br />

Cloudsandlight<br />

%yr 1<br />

Lightchange(+3<br />

to 3%)(1998<br />

2009)JUST<br />

BELOW<br />

sea(ice?)surface<br />

PP<strong>in</strong>crease<br />

(19982009)<br />

estimated<br />

belowsea<br />

(ice?)surface<br />

Bélanger etal.2012BGD


W<strong>in</strong>d!=>w<strong>in</strong>ddriventurbulenceand<br />

eddies=>mix<strong>in</strong>g,nitrateconsumption<br />

Withicevs.WithoutIce Woodgate,Ra<strong>in</strong>ville,Mahadevan,<br />

Wang,Matrai,<strong>in</strong>prep<br />

Muchtobedoneon<strong>the</strong>model<strong>in</strong>gside:<br />

AOMIP<br />

(http://www.whoi.edu/page.do?pid=29836)<br />

4 th <strong>Primary</strong>ProductionAlgorithmRoundRob<strong>in</strong><br />

(contactpmatrai@bigelow.org)


Summary<br />

• Seaiceisth<strong>in</strong>n<strong>in</strong>gandextentisreduced,especially<strong>in</strong>summer<br />

• <strong>Primary</strong><strong>production</strong>seasonisexpectedto<strong>in</strong>crease<strong>in</strong>duration<br />

(light)butnot<strong>in</strong>magnitude(nutrients)atpanarcticscales<br />

• <strong>Primary</strong><strong>production</strong>andproductivity<strong>in</strong>crease<strong>in</strong>certa<strong>in</strong><br />

cont<strong>in</strong>entalshelvesandbreaks; andmove=>Whose<br />

fisheries!?<br />

• <strong>Primary</strong><strong>production</strong>andproductivityisnotexpectedto<br />

<strong>in</strong>crease<strong>in</strong><strong>the</strong>deep<strong>Arctic</strong>Bas<strong>in</strong>(notenoughnutrients)<br />

• Theecosystemsof<strong>the</strong><strong>Arctic</strong><strong>Ocean</strong>willchange<strong>the</strong>irpresent<br />

dayequilibrium. Wedonotknowhow<strong>the</strong>newequilibrium<br />

willsupportecosystemservices<br />

• Ourpredictionsareonlyasgoodasourvalidat<strong>in</strong>gdataand<br />

processunderstand<strong>in</strong>gare


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