Gruber N, Doney SC, Emerson SR, Gilbert D, Kobayashi T, Kortzinger A, Johnson GC, Johnson
KJ, Riser SC, Ulloa O (2007) The argo-oxygen program. Argo Steering Committee
Halsey KH, Milligan AJ, Behrenfeld MJ (2010) Physiological optimization underlies growth rateindependent chlorophyll-specific gross and net primary production. Photosynth Res
103(2):125–137
Henson SA, Raitsos D, Dunne JP, McQuatters-Gollop A (2009) Decadal variability in
biogeochemical models: Comparison with a 50-year ocean colour dataset. Geophys Res Lett
36. doi:10.1029/2009gl040874
Hirata T, Aiken J, Hardman-Mountford N, Smyth TJ, Barlow RG (2008) An absorption model to
determine phytoplankton size classes from satellite ocean colour. Remote Sens Environ
112(6):3153–3159. doi:10.1016/j.rse.2008.03.011
Hovis WA, Clark DK, Anderson F, Austin RW, Wilson WH, Baker ET, Ball D, Gordon HR,
Mueller JL, El-Sayed SZ, Sturm B, Wrigley RC, Yentsch CS (1980) Nimbus-7 coastal zone
color scanner—system description and initial imagery. Science 210(4465):60–63
Howard KL, Yoder JA (1997) Contribution of the sub-tropical oceans to global primary
production. In: Liu C-T (ed) Proceedings of cospar colloquium on space remote sensing of
subtropical oceans. New York, pp 157–168
Johnson KS, Riser SC, Karl DM (2010) Nitrate supply from deep to near-surface waters of the
north pacific subtropical gyre. Nature 465(7301):1062–1065. doi:10.1038/nature09170
Kostadinov TS, Siegel DA, Maritorena S (2009) Retrieval of the particle size distribution from
satellite ocean color observations. J Geophys Res 114. doi:10.1029/2009jc005303
Kostadinov TS, Siegel DA, Maritorena S (2010) Global variability of phytoplankton functional
types from space: Assessment via the particle size distribution. Biogeosciences
7(10):3239–3257. doi:10.5194/bg-7-3239-2010
Laws EA, Bannister TT (1980) Nutrient-limited and light-limited growth of thalassiosirafluviatilis in continuous culture, with implications for phytoplankton growth in the ocean.
Limnol Oceanogr 25(3):457–473
Laws EA, Falkowski PG, Smith WO, Ducklow H, McCarthy JJ (2000) Temperature effects on
export production in the open ocean. Glob Biogeochem Cycles 14(4):1231–1246
Lee ZP, Carder KL, Arnone RA (2002) Deriving inherent optical properties from water color: a
multiband quasi-analytical algorithm for optically deep waters. Appl Opt 41(27):5755–5772
Lee ZP, Carder KL, Marra J, Steward RG, Perry MJ (1996) Estimating primary production at
depth from remote sensing. Appl Optics 35(3):463–474
Loisel H, Duforet L, Dessailly D, Chami M, Dubuisson P (2008) Investigation of the variations in
the water leaving polarized reflectance from the polder satellite data over two biogeochemical
contrasted oceanic areas. Opt Express 16(17):12905–12918. doi:10.1364/oe.16.012905
Longhurst A, Sathyendranath S, Platt T, Caverhill C (1995) An estimate of global primary
production in the ocean from satellite radiometer data. J Plankton Res 17:1245–1271
Lozier MS, Dave AC, Palter JB, Gerber LM, Barber RT (2011) On the relationship between
stratification and primary productivity in the north atlantic. Geophys Res Lett 38. doi:10.1029/
2011gl049414
Luz B, Barkan E (2009) Net and gross oxygen production from o-2/ar, o-17/o-16 and o-18/o-16
ratios. Aquat Microb Ecol 56(2–3):133–145. doi:10.3354/ame01296
Marra J (2009) Net and gross productivity: weighing in with (14)c. Aquat Microb Ecol
56(2–3):123–131. doi:10.3354/ame01306
Martinez E, Antoine D, D’’rtenzio F, Gentili B (2009) Climate-driven basin-scale decadal
oscillations of oceanic phytoplankton. Science 326(5957):1253–1256. doi:10.1126/
science.1177012
Milutinovic S, Bertino L (2011) Assessment and propagation of uncertainties in input terms
through an ocean-color-based model of primary productivity. Remote Sens Environ
115(8):1906–1917. doi:10.1016/j.rse.2011.03.013
Morel A (1991) Light and marine photosynthesis: a spectral model with geochemical and
climatological implications 26:263–306
228
T. K. Westberry and M. J. Behrenfeld
KJ, Riser SC, Ulloa O (2007) The argo-oxygen program. Argo Steering Committee
Halsey KH, Milligan AJ, Behrenfeld MJ (2010) Physiological optimization underlies growth rateindependent chlorophyll-specific gross and net primary production. Photosynth Res
103(2):125–137
Henson SA, Raitsos D, Dunne JP, McQuatters-Gollop A (2009) Decadal variability in
biogeochemical models: Comparison with a 50-year ocean colour dataset. Geophys Res Lett
36. doi:10.1029/2009gl040874
Hirata T, Aiken J, Hardman-Mountford N, Smyth TJ, Barlow RG (2008) An absorption model to
determine phytoplankton size classes from satellite ocean colour. Remote Sens Environ
112(6):3153–3159. doi:10.1016/j.rse.2008.03.011
Hovis WA, Clark DK, Anderson F, Austin RW, Wilson WH, Baker ET, Ball D, Gordon HR,
Mueller JL, El-Sayed SZ, Sturm B, Wrigley RC, Yentsch CS (1980) Nimbus-7 coastal zone
color scanner—system description and initial imagery. Science 210(4465):60–63
Howard KL, Yoder JA (1997) Contribution of the sub-tropical oceans to global primary
production. In: Liu C-T (ed) Proceedings of cospar colloquium on space remote sensing of
subtropical oceans. New York, pp 157–168
Johnson KS, Riser SC, Karl DM (2010) Nitrate supply from deep to near-surface waters of the
north pacific subtropical gyre. Nature 465(7301):1062–1065. doi:10.1038/nature09170
Kostadinov TS, Siegel DA, Maritorena S (2009) Retrieval of the particle size distribution from
satellite ocean color observations. J Geophys Res 114. doi:10.1029/2009jc005303
Kostadinov TS, Siegel DA, Maritorena S (2010) Global variability of phytoplankton functional
types from space: Assessment via the particle size distribution. Biogeosciences
7(10):3239–3257. doi:10.5194/bg-7-3239-2010
Laws EA, Bannister TT (1980) Nutrient-limited and light-limited growth of thalassiosirafluviatilis in continuous culture, with implications for phytoplankton growth in the ocean.
Limnol Oceanogr 25(3):457–473
Laws EA, Falkowski PG, Smith WO, Ducklow H, McCarthy JJ (2000) Temperature effects on
export production in the open ocean. Glob Biogeochem Cycles 14(4):1231–1246
Lee ZP, Carder KL, Arnone RA (2002) Deriving inherent optical properties from water color: a
multiband quasi-analytical algorithm for optically deep waters. Appl Opt 41(27):5755–5772
Lee ZP, Carder KL, Marra J, Steward RG, Perry MJ (1996) Estimating primary production at
depth from remote sensing. Appl Optics 35(3):463–474
Loisel H, Duforet L, Dessailly D, Chami M, Dubuisson P (2008) Investigation of the variations in
the water leaving polarized reflectance from the polder satellite data over two biogeochemical
contrasted oceanic areas. Opt Express 16(17):12905–12918. doi:10.1364/oe.16.012905
Longhurst A, Sathyendranath S, Platt T, Caverhill C (1995) An estimate of global primary
production in the ocean from satellite radiometer data. J Plankton Res 17:1245–1271
Lozier MS, Dave AC, Palter JB, Gerber LM, Barber RT (2011) On the relationship between
stratification and primary productivity in the north atlantic. Geophys Res Lett 38. doi:10.1029/
2011gl049414
Luz B, Barkan E (2009) Net and gross oxygen production from o-2/ar, o-17/o-16 and o-18/o-16
ratios. Aquat Microb Ecol 56(2–3):133–145. doi:10.3354/ame01296
Marra J (2009) Net and gross productivity: weighing in with (14)c. Aquat Microb Ecol
56(2–3):123–131. doi:10.3354/ame01306
Martinez E, Antoine D, D’’rtenzio F, Gentili B (2009) Climate-driven basin-scale decadal
oscillations of oceanic phytoplankton. Science 326(5957):1253–1256. doi:10.1126/
science.1177012
Milutinovic S, Bertino L (2011) Assessment and propagation of uncertainties in input terms
through an ocean-color-based model of primary productivity. Remote Sens Environ
115(8):1906–1917. doi:10.1016/j.rse.2011.03.013
Morel A (1991) Light and marine photosynthesis: a spectral model with geochemical and
climatological implications 26:263–306
228
T. K. Westberry and M. J. Behrenfeld