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A FUNDAMENTAL CHALLENGE IS TO PREDICT WHETHER NET PRIMARY PRODUCTION (NETPP) IN THIS REGION WILL INCREASE OR DECREASE UNDER CHANGING NORTHERLY AND SOUTHERLY ADVECTIVE FLOWS. HERE  WE SUGGEST THAT THE BALANCE WILL DEPEND ON REGIONAL BOTTOM-UP DRIVERS (E.G.  STRATIFICATION  NUTRIENT AND LIGHT AVAILABILITY  COMMUNITY COMPOSITION) AND TOP-DOWN DRIVERS (E.G.  GRAZING). A GROWING UNDERSTANDING OF THE SURFACE AND DEEP OVERFLOWS  COUNTERFLOWS  AND RECIRCULATION PATTERNS WITHIN THE SUBARCTIC ATLANTIC IS EMERGING THAT INDICATES STRONGER INFLUENCES OF THE ATLANTIC SURFACE WATER (AW) AND ARCTIC-ORIGIN WATER (ARW) ON EACH OTHER AND ON THE AVERAGE CIRCULATION PATTERNS WITHIN THE SUBARCTIC ATLANTIC THAN PREVIOUSLY THOUGHT. WE DEFINE THE SUBARCTIC ATLANTIC AS THE REGION ENCOMPASSED BY THE GREENLAND-ICELAND-NORWEGIAN (GIN)  IRMINGER AND LABRADOR SEAS  WHERE WARMER AND SALTIER AW LADEN WITH NUTRIENTS  PLANKTON AND DETRITUS MOVES NORTH IN MULTIPLE BRANCHES INTO THE LABRADOR SEA  INTO THE GIN SEAS AND  EVENTUALLY  INTO THE ARCTIC OCEAN. FRESHER AND COLDER ARW WITH SEA ICE  LOW NUTRIENTS  LOW PLANKTON AND HIGH COLORED DISSOLVED ORGANIC MATTER MOVES SOUTHWARDS ALONG THE EDGE OF THE EASTERN GREENLAND AND WESTERN LABRADOR SEAS AND INTO THE N. ATLANTIC. HERE  WE WILL FOCUS ON THE BALANCE OF NETPP IN THE SUBARCTIC ATLANTIC AS AFFECTED BY (I) ADVECTIVE LOSSES AND GAINS WITHIN THIS REGION AT LARGE-SCALES INTERACTION WITH RESPECT TO BOUNDARY CONDITIONS IN THE TEMPERATE N. ATLANTIC AND ARCTIC OCEANS; (II) LATERAL AND VERTICAL EXPORT PRODUCTION WITHIN SUB-REGIONS OF THE SUBARCTIC ATLANTIC AT INTERMEDIATE SCALES; AND (III) ADVECTIVE AND LOCAL PROCESSES CONTROLLING NETPP IN THE SUBARCTIC ATLANTIC REGION. OUR QUESTIONS INCLUDE THE FOLLOWING: (Q1) WHAT BOTTOM-UP (PHYSICAL AND CHEMICAL) FACTORS CONTROL THE NETPP LEVELS IN THE SUBARCTIC ATLANTIC  WHERE AND WHEN? (Q2) WHAT ARE THE CONTROLS OF SEASONAL AND SUB-SEASONAL VARIABILITIES AND TRENDS IN THE SUBARCTIC ATLANTIC? (Q3) WHAT IS THE BALANCE BETWEEN LOCAL AND ADVECTED NETPP IN THE SUBARCTIC ATLANTIC DURING THE GROWTH SEASON? WE PROPOSE TO USE A HIERARCHY OF MODELS INCLUDING A FULL 3D  COUPLED  BIOGEOCHEMICAL-PHYSICAL MODEL AT REGIONAL SCALE (SINMOD) AND A SPECIALIZED 1D SATELLITE OCEAN COLOR MODEL FOR PHYTOPLANKTON NETPP (UQAR-TAKUVIK)  BOTH OF WHICH ARE EXCEPTIONALLY WELL TUNED TO HIGH LATITUDES. MODEL SIMULATIONS WILL BE DONE IN CONCERT WITH MINING HISTORICAL FIELD AND SATELLITE DATA TO BETTER UNDERSTAND THE TEMPORAL EVOLUTION OF NETPP AND ITS PHYSICAL AND ECOLOGICAL CONTROLS OVER AN AVERAGE ANNUAL CYCLE IN THE SUBARCTIC ATLANTIC. 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