Skip to main content
Log in

Spike in phytoplankton biomass in Greenland Sea during 2009 and the correlations among chlorophyll-a, aerosol optical depth and ice cover

  • Biology
  • Published:
Chinese Journal of Oceanology and Limnology Aims and scope Submit manuscript

Abstract

The distributions and correlations of chlorophyll-a (Chl-a), aerosol optical depth (AOD) and ice cover in the southeast Arctic Ocean-Greenland Sea (10°W–10°E, 70°–80°N) between 2003 and 2009 were studied using satellite data and statistical analyses. Regression analysis showed correlations between Chl-a and AOD, Chl-a and ice cover, and AOD and ice cover with different time lags. The time lag of Chl-a and AOD indicated their long-term equilibrium relationship. Peaks in AOD and Chl-a and generally occurred in May and July, respectively. Despite the time lag, the correlation between Chl-a and AOD in the study region was as high as 0.7. The peak gap between Chl-a and AOD shifted for about 6 weeks during 2003–2009. In the summer and autumn of 2009, Chl-a and AOD levels were much higher than during the other years, especially in the northern band of the study region (75°–80°N). The driving forces for this localized increase in phytoplankton biomass could be mainly attributed to the very high rate of ice melting in spring and early summer and the high wind speed in autumn, together with the increased deposition of aerosol throughout the year. The unusually high AOD in the spring of 2003 was mainly due to a massive fire in Russia, which occurred in the first half of the year. Over the 7 years of the study, the sea surface temperature generally decreased. This may have been due to the release of dimethylsulfide into the air, excreted in large amounts from abundant phytoplankton biomass, and its subsequent reaction, form large amounts of aerosol, and resulting in regional cooling.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Aagaard K, Coachman L K. 1968. The East Greenland Current north of Denmark Strait, Part I. Arctic, 21: 181–200.

    Google Scholar 

  • Becker V, Huszar V L M, Naselli-Flores L, and Padisak J. 2008. Phytoplankton equilibrium phases during thermal stratification in a deep subtropical reservoir. Freshwater Biology, 53: 952–963.

    Article  Google Scholar 

  • Carol M L, Timothy P. 2004. Biological Oceanography: An Introduction. ISBN 9780750633840. http://www.somas.stonybrook.edu/~conover/Textbooks/Biological%20Oceanography.pdf.

    Google Scholar 

  • Charlson R J, Lovelock J E, Andreae M O, Warren S G. 1987. Oceanic phytoplankton, atmospheric sulphur, cloud albedo and climate. Nature, 326: 655–661.

    Article  Google Scholar 

  • Chisholm S W, Morel F M M. 1991. What controls phytoplankton production in nutrient-rich areas of the open sea?. Limnol. Oceanogr., 36: 1 507–1 970.

    Article  Google Scholar 

  • Cota C F. 1994. Phytosynthesis of haeocystis in the Greenland Sea. Limnol. Oceanogr., 39(4): 948–953.

    Article  Google Scholar 

  • Cropp R A, Gabric A J, McTainsh G H, Braddock R D, Tindale N W. 2005. Coupling between ocean biota and atmospheric aerosols: dust, DMS or artefact?. Global Biogeochemical Cycles, 19: GB4002.

    Article  Google Scholar 

  • Fahnenstiel G A, Pothoven S, Nalepa T, Vanderploeg H, Klarer D, Scavia D. 2010. Recent changes in primary production and phytoplankton in the offshore region of southeastern Lake Michigan. J. Great Lakes Res., 36(Suppl. 3): 20–29.

    Article  Google Scholar 

  • Gabric A J, Cropp R, Ayers G P, McTainsh G, Branddock R. 2002. Coupling between cycles of phytoplankton biomass and aerosol optical depth as derived from SeaWiFS time series in the Subantarctic Southern Ocean. Geophys. Res. Lett., 29(7): 1 112–1 146.

    Article  Google Scholar 

  • Gabric A J, Gregg W, Najjar R, Erickson D, Matrai P. 2001. Modelling the biogeochemical cycle of simethylsulfide in the upper ocean: a review. Chemosphere-Global Change.Science, 126: 1–16.

    Google Scholar 

  • Gabric A J, Murray N, Stone L, Koh M. 1993. Modelling the production of dimethylsulfide during a phytoplankton bloom. Journal of Geophysical Research — Ocean, 9: 822, 805–822, 816.

    Google Scholar 

  • Gabric A J, Shephard J M, Knight J M, Jones G B, Trevena A J. 2005. Correlations between the satellite-derived seasonal cycles of phytoplankton biomass and aerosol optical depth in the Southern Ocean: evidence for the influence of sea ice. Global Biogeochemical Cycles, 19: 1–10.

    Article  Google Scholar 

  • Generoso S, Bey I, Attié J L, Bréon F M. 2007. A satellite- and model-based assessment of the 2003 Russian fires: impact on the Arctic region. J. Geophys. Res., 112: D15302, http://dx.doi.org/10.1029/2006JD008344.

    Article  Google Scholar 

  • Heide-Jørgensen M P, Laidre K L, Logsdon M L, Nielsen T G. 2007. Springtime coupling between phytoplankton, sea ice and sea temperature in Disko Bay, West Greenland. Progress in Oceanography, 73: 79–95.

    Article  Google Scholar 

  • Horner R A. 1985. Ecology of sea ice microalgae.In: Horner R A ed. Sea Ice Biota. CRC Press. p.83–103.

  • Hunt G L, Jr Drinkwater K F. 2005. Background on the climatology, physical oceanography and exosystems of the sub-Arctic Seas. Appendix to the ESSAS Science Plan. GLOBEC Report, No.20, viii, 96.

    Google Scholar 

  • Hurrell J W. 2000. The North Atlantic Oscillation. Prepared for the National Academy of Sciences, 12th Annual Symposium on Frontiers of Science, Irvine, CA.

    Google Scholar 

  • Ikavalko J, Gradinger R. 1997. Flagellates and heliozoans in the Greenland Sea ice studies alive using light microscopy. Polar Biology, 17: 473–481.

    Article  Google Scholar 

  • Jones I D, Elliott A. 2007. Modelling the effect of changing retention time on abundance and composition of phytoplankton species in a small lake. Freshw. Biol., 52: 988–997.

    Article  Google Scholar 

  • Kahru M, Gille S T, Murtugudde R, Strutton P G, Manzano-Sarabia M, Wang H, Mitchell B G. 2010. Global correlations between winds and ocean chlorophyll. Journal of Geophysical Research, 115(C12): L1–11, http://dx.doi.org/10.1029/2010JC006500.

    Article  Google Scholar 

  • Kulmala M, Riipinen I, Sipila M, Manninen H E, Petaja T, Junninen H, Maso M D, Mordas G, Mirme A, Vana M, Hirsikko A, Laakso L, Harrison R M, Hanson I, Leung C, Lehtinen K E J, Kerminen V-M. 2007. Toward direct measurement of atmospheric nucleation. Science, 318: 89–92.

    Article  Google Scholar 

  • Lara R J, Kattner G, Tillmann U, Hirche H J. 1994. The North East Water polynya (Greenland Sea) II. Mechanisms of nutrient supply and influence on phytoplankton distribution. Polar Biol., 14: 483–490.

    Article  Google Scholar 

  • Loose B, Miller L A, Elliott S, Papakyriakou T. 2011. Sea ice biogeochemistry and material transport across the frozen interface. Oceanography, 24(3): 202–218.

    Article  Google Scholar 

  • Matrai P A, Vernet M. 1997. Dynamics of the vernal bloom in the marginal ice zone of the Barents Sea: dimethylsulfide and dimethysulfoniopropionate budgets. Journal of Geophysical Research—Ocean, 102: 22 965–22 979.

    Article  Google Scholar 

  • Qu B, Gabric A J, Zhu J N, Lin D R, Qian F, Zhao M. 2012. Correlation between sea surface temperature and wind speed in Greenland Sea and their relationships with NAO variability. Water Science and Engineering, 5(3): 304–315.

    Google Scholar 

  • Qu B, Gabric A J. 2010. Using genetic algorithms to calibrate a dimethylsulfide production model in the Arctic Ocean. Chinese Journal of Oceanology and Limnology, 28(1): 1–10, http://dx.doi.org/10.1007/s00343-010-9062-x.

    Article  Google Scholar 

  • Rangel L M, Silva L H S, Rosa P, Roland F, Huszar V L M. 2012. Phytoplankton biomass is mainly controlled by hydrology and phosphorus concentrations in tropical hydroelectric reservoirs. Hydrobiologia, 693: 13–28.

    Article  Google Scholar 

  • Rey F, Noji T T, Mille L A. 2000. Seasonal phytoplankton development and new production in the central Greenland Sea. Sarsia, 85: 329–344.

    Google Scholar 

  • Siegel D A, Doney S C, Yoder J A. 2002. The North Atlantic spring phytoplankton bloom and Sverdrup’s critical depth hypothesis. Science, 296: 730–733.

    Article  Google Scholar 

  • Spreen G, Kern S, Stammer D, Hansen E. 2009. Fram Strait sea ice volume export estimated between 2003 and 2008 from satellite data. Geophysical Research Letters, 36: L19502, http://dx.doi.org/20.1029/2009GL039591.

    Article  Google Scholar 

  • Struthers H, Ekman A M L, Glantz P, Iversen T, Kirkevåg A, Mårtensson E M, Selø, Nilsson E D. 2011. The effect of sea ice loss on sea salt aerosol concentrations and the radiative balance in the Arctic. Atmos. Chem. Phys., 11: 3 459–3 477, http://dx.doi.org/10.5194/acp-11-3459-2011.

    Article  Google Scholar 

  • Svend-Aage M, Steingrimur J. 1997. Timing of deep convection in the Greenland and Iceland Seas. Journal of Marine Science, 54: 300–309.

    Google Scholar 

  • Thomas D N, Dieckmann G S eds. 2010. Sea Ice. 2nd edn. Siley-Blackwell, Oxford IK. p.640.

    Google Scholar 

  • Tsuknerik M, Deser C, Alexander M, Tomas R. 2010. Atmospheric forcing of Fram Strait sea ice export: a closer look. Climate Dynamics, 35(7): 1 349–1 360.

    Google Scholar 

  • Werner I, Ikavalko J, Schunemann H. 2007. Sea-ice algae in Arctic pack ice during later winter. Polar Biol., 30: 1 493–1 504.

    Article  Google Scholar 

  • Woodgate R A, Fahrbach E, Rohardt G. 1999. Structure and transport of the East Greenland Current at 75°N from moored current meters. Journal of Geophysical Research, 104: 18 059–18 072.

    Article  Google Scholar 

  • Yager P, Wallace D, Johnson K, Smith W, Minnett P, Deming J. 1995. The Northeast Water Polynya as an atmospheric CO2 sink: a seasonal rectification hypothesis. Journal of Geophysical Research, 100(C3), http://dx.doi.org/10.1029/94JC01962.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Bo Qu  (瞿波).

Additional information

Supported by the National Natural Science Foundation of China (No. 41276097)

Rights and permissions

Reprints and permissions

About this article

Cite this article

Qu, B., Gabric, A.J., Lu, H. et al. Spike in phytoplankton biomass in Greenland Sea during 2009 and the correlations among chlorophyll-a, aerosol optical depth and ice cover. Chin. J. Ocean. Limnol. 32, 241–254 (2014). https://doi.org/10.1007/s00343-014-3141-3

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00343-014-3141-3

Keyword

Navigation