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References

  • Aagaard, K., J. D. Schumacher, and A. T. Roach (1985), On the wind-driven flow through Bering Strait, J. Geophys. Res., 90, 72137221.
  • Bates, N. R., A. F. Michaels, and A. H. Knap (1996), Seasonal and interannual variability of oceanic carbon dioxide species at the U.S. JGOFS Bermuda Atlantic Time-series Study (BATS) site, Deep Sea Res., Part II, 43, 347383.
  • Beer, T. (1983), Environmental Oceanography. Textbook to “The Applied Environmetrics Oceanographical Tables”, pp. 117129, Elsevier, New York.
  • Bond, N. A., and J. M. Adams (2002), Atmospheric forcing of the southeastern Bering Sea shelf during 1995–1999 in the context of a 40-year historical record, Deep Sea Res., Part II, 49, 58695887.
  • Borges, A. V., and M. Frankignoulle (2001), Short-term variations of the partial pressure of CO2 in surface waters of the Galician upwelling system, Prog. Oceanogr., 51(2–4), 283302.
  • Borges, A. V., and M. Frankignoulle (2002), Distribution of surface carbon dioxide and air-sea exchange in the upwelling system off the Galician coast, Global Biogeochem. Cycles, 16(2), 1020, doi:10.1029/2000GB001385.
  • Chen, C.-T. A., A. Andreev, K.-R. Kim, and M. Yamamoto (2004), Roles of continental shelves and marginal seas in the biogeochemical cycles of the North Pacific Ocean, J. Oceanogr., 60, 1744.
  • Chierici, M., A. Fransson, and Y. Nojiri (2004), Biological and physical processes as drivers of the seasonal surface water pCO2 in different domains of the subarctic North Pacific, paper presented at Institute of Ocean Sciences Seminar Series, B. C., Canada, 7 June.
  • Chierici, M., A. Fransson, and Y. Nojiri (2006), Biogeochemical processes as drivers of surface fCO2 in contrasting provinces in the subarctic North Pacific Ocean, Global Biogeochem. Cycles, 20, GB1009, doi:10.1029/2004GB002356.
  • Cokelet, E. D., M. L. Schall, and D. Dougherty (1996), ADCP-referenced geostrophic circulation in the Bering Sea basin, J. Phys. Oceanogr., 26, 11131128.
  • de Boyer Montégut, C., G. Madec, A. S. Fisher, A. Lazar, and D. Iudicone (2004), Mixed layer depth over the global ocean: An examination of profile data and a profile-based climatology, J. Geophys. Res., 109, C12003, doi:10.1029/2004JC002378.
  • Denman, K. L., and A. E. Gargett (1988), Multiple thermoclines are barriers to vertical exchange in the subarctic Pacific during SUPER, May 1984, J. Mar. Res., 46, 77103.
  • Dickson, A. G., and C. Goyet (Eds.) (1994), DOE handbook of methods for the analysis of the various parameters of the carbon dioxide system in sea water, version 2, Rep. ORNL/CDIAC-74, Carbon Dioxide Inf. Anal. Cent., Oak Ridge Natl. Lab., Oak Ridge, Tenn.
  • Dickson, A. G., and F. J. Millero (1987), A comparison of the equilibrium constants for the dissociation of carbonic acid in seawater media, Deep Sea Res., Part I, 34, 17331743.
  • Favorite, F. A., A.-J. Dodimead, and K. Nasu (1976), Oceanography of the subarctic Pacific region, 1960–71, Bull. Int. North Pac. Fish. Comm., 33, 187.
  • Gago, J., X. A. Alvarez-Salgado, F. F. Perez, and A. F. Rios (2003), Partitioning of physical and biogeochemical contributions to short-term variability of pCO2 in a coastal upwelling system: A quantitative approach, Mar. Ecol. Prog. Ser., 255, 4354.
  • Gardner, J. V. (2003), Report on the LOTS cruise to map foot of the slope and 2500-m isobath of Bowers Ridge and Beringian margin, Bering Sea July 7, to July 28, 2003 Dutch Harbor, AK to Dutch Harbor, AK, Cent. for Coastal and Ocean Mapp./Joint Hydrogr. Cent., Univ. of N. H., Durham. (Available at http://www.ccomjhc.unh.edu/unclos/html/report_beringsea.htm#c).
  • Goes, J. I., H. D. R. Gomes, A. Limsakul, and T. Saino (2004), The influence of large scale environmental changes on carbon export in the North Pacific Ocean using satellite and shipboard data, Deep Sea Res., Part II, 51(1–3), 247279.
  • Gonzalez-Davila, M., J. M. Santana-Casiano, M. J. Rueda, O. Llinas, and E. F. Gonzalez-Davila (2003), Seasonal and interannual variability of sea-surface carbon dioxide species at the European Station for Time Series in the Ocean at the Canary Islands (ESTOC) between 1996 and 2000, Global Biogeochem. Cycles, 17(3), 1076, doi:10.1029/2002GB001993.
  • Harashima, A., R. Tsuda, Y. Tanaka, T. Kimoto, H. Tatsuta, and K. Furusawa (1997), Monitoring algal blooms and related biogeochemical changes with a flow-through system deployed on ferries in the adjacent seas of Japan, in Monitoring Algal Blooms: New Techniques for Detecting Large-Scale Environmental Change, edited by M. Kahru, and C. Brown, pp. 85112, Springer, New York.
  • Hermann, A. J., P. J. Stabeno, D. B. Haidvogel, and D. L. Musgrave (2002), A regional tidal/subtidal circulation model of the southeastern Bering Sea: Development, sensitivity and hindcasting, Deep Sea Res., Part II, 49, 59455967.
  • Hollowed, A. (Ed.) (1996), Report on climate change and carrying capacity of the North Pacific ecosystem, Rep. 15, 95 pp., Sci. Steering Comm. Coord. Off., U.S. Global Ocean Ecosyst. Dyn. (GLOBEC), Dep. of Integrative Biol., Univ. of Calif., Berkeley.
  • Hunt, G. L.Jr., P. Stabeno, G. Walters, E. Sinclair, R. D. Brodeur, J. M. Napp, and N. A. Bond (2002), Climate change and control of the southeastern Bering Sea pelagic ecosystem, Deep Sea Res., Part II, 49, 58215853.
  • Ianson, D., and S. E. Allen (2002), A two-dimensional nitrogen and carbon flux model in a coastal upwelling region, Global Biogeochem. Cycles, 16(1), 1011, doi:10.1029/2001GB001451.
  • Ianson, D., S. E. Allen, S. L. Harris, K. J. Orians, D. E. Varela, and C. S. Wong (2003), The inorganic carbon system in the coastal upwelling region west of Vancouver Island, Canada, Deep Sea Res., Part I, 50, 10231042.
  • Inoue, H. Y., H. Matsueda, M. Ishii, K. Fushimi, M. Hirota, I. Asanuma, and Y. Takasugi (1995), Long term trend of the partial pressure of carbon dioxide (pCO2) in surface waters of the western North Pacific, 1984–1993, Tellus, Ser. B, 47, 391413.
  • Keeling, C. D., and T. P. Whorf (2004), Atmospheric CO2 records from sites in the SIO air sampling network, in Trends: A Compendium of Data on Global Change, Carbon Dioxide Inf. Anal. Cent., Oak Ridge Natl. Lab., U.S. Dep. of Energy, Oak Ridge, Tenn. (Available at http://cdiac.ornl.gov/ftp/trends/co2/maunaloa.co2).
  • Kimoto, T., and A. Harashima (1993), High resolution time/space monitoring of the surface seawater CO2 partial pressure by ship-of-opportunity, paper presented at Fourth International Carbon Dioxide Conference, Carqueiranne, France.
  • Körtzinger, A., H. Thomas, B. Schneider, N. Gronau, L. Mintrop, and J. C. Duinker (1996), At-sea intercomparison of two newly designed underway pCO2 systems - Encouraging results, Mar. Chem., 52, 133145.
  • Lefèvre, N., A. J. Watson, A. Olsen, A. F. Ríos, F. F. Pérez, and T. Johannssen (2004), A decrease in the sink of atmospheric CO2 in the North Atlantic, Geophys. Res. Lett., 31, L07306, doi:10.1029/2003GL018957.
  • Le Quéré, C., O. Aumont, P. Monfray, and J. Orr (2003), Propagation of climate events on surface stratification, marine biology and CO2: Case studies over the 1979–1999 period, J. Geophys. Res., 108(C12), 3375, doi:10.1029/2001JC000920.
  • Lewis, E., and D. W. R. Wallace (1998), Program developed for CO2 system calculations, ORNL/CDIAC-105, Carbon Dioxide Inf. Anal. Cent., Oak Ridge Natl. Lab., U.S. Dep. of Energy, Oak Ridge, Tenn.
  • Liss, P. S., and L. Merlivat (1986), Air-sea gas exchange rates: Introduction and synthesis, in The Role of Air-Sea Exchange in Geochemical Cycling, edited by P. Baut-Menard, NATO ASI Ser., Ser. C, Math. Phys. Sci., 185, 113128.
  • Liu, H., K. Suzuki, and T. Saino (2002), Phytoplankton growth and microzooplankton grazing in the subarctic Pacific Ocean and the Bering Sea during summer 1999, Deep Sea Res., Part I, 49, 363375.
  • Luchin, V. A., V. A. Menovshchikov, V. M. Lavrentiev, and R. K. Reed (1999), Thermohaline structure of water masses in the Bering Sea, in Dynamics in the Bering Sea, edited by T. R. Loughlin, and K. Othani, pp. 128, Univ. of Alaska Sea Grant, Fairbanks.
  • Macklin, S. A., G. L. Hunt, and J. E. Overland (2002), Collaborative research on the pelagic ecosystem of the southeastern Bering Sea shelf, Deep Sea Res., Part II, 49, 58135819.
  • Mehrbach, C., C. H. Culberson, J. E. Hawley, and R. M. Pytkowicz (1973), Measurement of the apparent dissociation constants for carbonic acid in seawater at atmospheric pressure, Limnol. Oceanogr., 18, 897907.
  • Midorikawa, T., K. Ogawa, K. Nemoto, H. Kamiya, T. Umeda, N. Hiraishi, A. Wada, and M. Ishii (2003), Interannual variations of net community production and air-sea CO2 flux from winter to spring in the western subarctic North Pacific, Tellus, Ser. B, 55, 466477.
  • Midorikawa, T., K. Nemoto, H. Kamiya, M. Ishii, and H. Inoue (2005), Persistently strong oceanic CO2 sink in the western subtropical North Pacific, Geophys. Res. Lett., 32, L05612, doi:10.1029/2004GL021952.
  • Minobe, S., and N. Mantua (1999), Interdecadal modulation of interannual atmospheric and oceanic variability over the North Pacific, Prog. Oceanogr., 43, 163192.
  • Miura, T., T. Suga, and K. Hanawa (2002), Winter mixed layer and formation of dichothermal water in the Bering Sea, J. Oceanogr., 58, 815823.
  • Murata, A., and T. Takizawa (2002), Impact of a coccolithophorid bloom on the CO2 system in surface waters of the eastern Bering Sea shelf, Geophys. Res. Lett., 29(11), 1547, doi:10.1029/2001GL013906.
  • Murphy, P. P., K. C. Kelly, R. A. Feely, and R. H. Gammon (1995), Carbon dioxide in surface water and the atmosphere during 1986–1989 NOAA/PMEL cruises in the Pacific and Indian Oceans, ORNDL/CDIAC-75, NDP-047, Oak Ridge Natl. Lab., Oak Ridge, Tenn.
  • Murphy, P. P., Y. Nojiri, Y. Fujinuma, C. S. Wong, J. Zeng, T. Kimoto, and H. Kimoto (2001), Measurements of surface water fCO2 from volunteer commercial ships: Techniques and experience from Skaugran, J. Atmos. Oceanic Technol., 18, 17191734.
  • Niebauer, H. J., V. Alexander, and S. Henrichs (1990), Physical and biological oceanographic interaction in the spring bloom at the Bering Sea marginal ice zone, J. Geophys. Res., 95, 22,22922,241.
  • Overland, J. E., and N. A. Adams (2001), North Pacific atmospheric and SST anomalies in 1997: Links to ENSO? Fish. Oceanogr., 10, 6980.
  • Overland, J. E., M. C. Spillane, H. E. Hulburt, and A. J. Wallcraft (1994), A numerical study of circulation of the Bering Sea basin exchange with the North Pacific Ocean, J. Phys. Oceanogr., 24, 736758.
  • Overland, J. E., J. M. Adams, and N. A. Bond (1999), Decadal variability of the Aleutian Low and its relation to high-latitude circulation, J. Clim., 12, 15421548.
  • Overland, J. E., N. A. Bond, and J. M. Adams (2002), The relation of surface forcing of the Bering Sea to large-scale climate patterns, Deep Sea Res., Part II, 49, 58555868.
  • Reed, R. K., and P. J. Stabeno (1994), Flow along and across the net Aleutian Ridge, J. Mar. Res., 52, 639648.
  • Reed, R. K., and P. J. Stabeno (1997), Long-term measurements of flow near the Aleutian Islands, J. Mar. Res., 55, 565575.
  • Reed, R. K., G. V. Khen, P. J. Stabeno, and A. V. Verkhunov (1993), Water properties and flow over the deep Bering Sea, summer 1991, Deep Sea Res., 40, 23252334.
  • Roden, G. I. (1995), Aleutian basin of the Bering Sea: Thermohaline, oxygen nutrient and current structure in July 1993, J. Geophys. Res., 100, 13,53913,554.
  • Royer, T. C., and M. Dagg (2002), Ecology of the southeastern Bering Sea, Deep Sea Res., Part II, 49, 5809.
  • Royer, T. C., and W. I. Emery (1984), Circulation in the Bering Sea, 1982–1983, based on satellite-tracked drifter observations, J. Phys. Oceanogr., 14, 19141920.
  • Rutllant, J. A., I. Masotti, J. Calderon, and S. A. Vega (2004), A comparison of spring coastal upwelling off central Chile at the extremes of the 1996–1997 ENSO cycle, Cont. Shelf Res., 24(7–8), 773787.
  • Schumacher, J. D., and V. Alexander (1999), Variability and role of the physical environment in the Bering Sea ecosystem, in Dynamics in the Bering Sea, edited by T. R. Loughlin, and K. Othani, pp. 147160, Univ. of Alaska Sea Grant, Fairbanks.
  • Shiomoto, A., E.-I. Saitoh, K. Imai, M. Toratani, Y. Ishida, and K. Sasaoka (2002), Interannual variation in phytoplankton biomass in the Bering Sea basin in the 1990s, Prog. Oceanogr., 55, 147163.
  • Stabeno, P. J., and R. K. Reed (1992), A major circulation anomaly in the western Bering Sea, Geophys. Res. Lett., 19, 16711674.
  • Stabeno, P. J., and R. K. Reed (1994), Circulation in the Bering Sea basin observed by satellite tracked drifters: 1986–1993, J. Phys. Oceanogr., 24, 848854.
  • Stabeno, P. J., J. D. Schumacher, and K. Ohtani (1999), The physical oceanography of the Bering Sea, in Dynamics in the Bering Sea, edited by T. R. Loughlin, and K. Othani, pp. 128, Univ. of Alaska Sea Grant, Fairbanks.
  • Stabeno, P. J., N. A. Bond, N. B. Kachel, S. A. Salo, and J. D. Schumacher (2001), On the temporal variability of the physical environment over the south-eastern Bering Sea, Fish. Oceanogr., 10(1), 8198.
  • Stabeno, P. J., N. B. Kachel, M. Sullivan, and T. E. Whitledge (2002), Variability of physical and chemical characteristics along the 70-m isobath of the southeastern Bering Sea, Deep Sea Res., Part II, 49, 59315943.
  • Stabeno, P. J., D. G. Kachel, N. B. Kachel, and M. E. Sullivan (2005), Observations from moorings in the Aleutian Passes: Temperature, salinity and transport, Fish. Oceanogr., 14, 1.
  • Takahashi, K. (1986), Seasonal fluxes of the pelagic diatoms in the subarctic Pacific, 1982–1983, Deep Sea Res., Part I, 33, 12251251.
  • Takahashi, K., N. Fujitani, and M. Yanada (2002), Long term monitoring of the particle fluxes in the Bering Sea and the central subarctic Pacific Ocean, 1990–2000, Prog. Oceanogr., 55, 95112.
  • Takahashi, T., J. Olafsson, J. G. Goddard, D. W. Chipman, and S. C. Sutherland (1993), Seasonal variation of CO2 and nutrients in the high latitude surface oceans: A comparative study, Global Biogeochem. Cycles, 7, 843878.
  • Torres, R., D. R. Turner, J. Rutllant, M. Sobarzo, T. Antezana, and H. E. Gonzales (2002), CO2-outgassing off central Chile (31–30 degrees S) and northern Chile (24–23 degrees S) during austral summer 1997: The effect of wind intensity on the upwelling and ventilation of CO2-rich waters, Deep Sea Res., Part II, 49(8), 14131429.
  • Torres, R., D. R. Turner, J. Rutllant, and N. Lefevre (2003), Continued CO2 outgassing in an upwelling area off northern Chile during the development phase of El Nino 1997–1998 (July 1997), J. Geophys. Res., 108(C10), 3336, doi:10.1029/2000JC000569.
  • Trenberth, K. E., and J. W. Hurrell (1994), Decadal atmosphere-ocean variations in the Pacific, Clim. Dyn., 9, 303319.
  • Vance, T. C., et al. (1998), Aqua-marine waters recorded for the first time in eastern Bering Sea, Eos Trans. AGU, 79(10), 121126.
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  • van Geen, A., R. K. Takesue, J. Goddard, T. Takahashi, J. A. Barth, and R. L. Smith (2000), Carbon and nutrient dynamics during coastal upwelling off Cape Blanco, Oregon, Deep Sea Res., Part II, 47(5–6), 9751002.
  • Walsh, J. J. (1991), Importance of continental margins in the marine biogeochemical cycling of carbon and nitrogen, Nature, 350, 5355.
  • Walsh, J. J., et al. (1989), Carbon and nitrogen cycling with the Bering/Chukchi Seas: Source regions for organic matter effecting AOU demands of the Arctic Ocean, Prog. Oceanogr., 22, 277359.
  • Wanninkhof, R. H. (1992), The relationship between wind speed and gas exchange over the ocean, J. Geophys. Res., 97, 73737382.
  • Wanninkhof, R., and W. R. McGillis (1999), A cubic relationship between air-sea CO2 exchange and wind speed, Geophys. Res. Lett., 26, 18891892.
  • Watai, T., M. Kikuchi, and T. Nakazawa (1998), Temporal variations of surface oceanic and atmospheric CO2 fugacity and dissolved inorganic carbon in the northwestern North Pacific, J. Oceanogr., 54, 323336.
  • Weiss, R. F. (1974), Carbon dioxide in water and seawater: The solubility of a non-ideal gas, Mar. Chem., 2, 203205.
  • Whitney, F. A., and D. W. Welch (2002), Impact of the 1997–1998 El Niño and 1999 La Niña on nutrient supply in the Gulf of Alaska, Prog. Oceanogr., 54, 405421.
  • Winn, C. D., Y.-H. Li, F. T. Mackenzie, and D. M. Karl (1998), Rising surface ocean dissolved inorganic carbon at the Hawaii Ocean Time-series site, Mar. Chem., 60, 3347.
  • Wong, C. S., F. A. Whitney, D. W. Crawford, and K. Iseki (1998), Enhancement of new production in the northeast subarctic Pacific Ocean during negative North Pacific index events, Limnol. Oceanogr., 43, 14181426.
  • Wong, C. S., N. A. D. Waser, Y. Nojiri, F. A. Whitney, J. S. Page, and J. Zeng (2002a), Seasonal cycles of nutrients and dissolved inorganic carbon at high and mid latitudes in the North Pacific Ocean during the Skaugran cruises: Determination of new production and nutrient uptake ratios, Deep Sea Res., Part II, 49, 53175338.
  • Wong, C. S., N. A. D. Waser, Y. Nojiri, K. W. Johnson, F. A. Whitney, J. C. S. Page, and J. Zeng (2002b), Seasonal and interannual variability in the distribution of surface nutrients and dissolved inorganic carbon in the northern North Pacific: Influence of El Niño, J. Oceanogr., 58, 227243.
  • Zeng, J., Y. Nojiri, P. P. Murphy, C. S. Wong, and Y. Fujinuma (2002), A comparison of ΔpCO2 distribution in the northern North Pacific using results from a commercial vessel in 1995–1999, Deep Sea Res., Part II, 49, 53035315.