484
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Deep-Sea Res. II. 43, 835–870.
Chavez, F.P., et al. (2003) From anchovies to sardines and back: multidecadal change in the Pacific
Ocean. Science. 299, 217–221.
Chelton, D.B. (1982) Large-scale response of the California Current to forcing by the wind stress
curl. Rept. Calif. Coop. Fish. Invest. 23, 130–148.
Chelton, D.B., and M.G. Schlax (1996) Global observations of oceanic Rossby waves. Science. 272,
234–238.
Chelton, D.B., et al. (1982) Large-scale interannual physical and biological interaction in the
California Current. J. Mar. Res. 40, 1095–1125.
Chen, S., and B. Qiu (2004) Seasonal variability of the South Equatorial Countercurrent. J. Geophys.
Res. 109, C08003.
Chen, Y.-L. (2000) Comparisons of primary productivity and phytoplankton size structure in the
marginal regions of southern East China Sea. Cont. Shelf Res. 20, 437–458.
Chen, Y.-L., et al. (2001) New production in the East China Sea, comparison between well-mixed
winter and stratified summer conditions. Cont. Shelf Res. 21, 751–764.
Chen, Y.-L., et al. (2004) Phytoplankton production during a summer coastal upwelling in the East
China Sea. Cont. Shelf Res. 24, 1321–1338.
Chen, Z., et al. (1992) The effects of a Kuroshio frontal eddy on the biochemical structure of the
East China Sea. In—Essays on the Investigation of the Kuroshio 4, pp. 115–124. China Ocean
Press, Beijing.
Chester, R. (2000) Marine Chemistry—Trace Elements in the Ocean, p. 522. Blackwell, Oxford.
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Chisholm, S.W. (1992) Phytoplankton size. In—Primary Productivity and Biogeochemical Cycles in
the Sea (P. G. Falkowski and A. D. Woodhead, Eds.), pp. 213–237. Plenum Press, New York.
Chisholm, S.W., et al. (1988) A novel free-living prochlorophyte abundant in the oceanic photic
zone. Nature, Lond. 334, 340–343.
Christian J.R., et al. (2002) Biogeochemical modelling of the tropical Pacific Ocean. II. Iron
geochemistry. Deep-Sea Res. II. 49, 545–556.
Christian, J.R., et al. (2004) A ribbon of dark water: phytoplankton blooms in the meanders of the
Pacific North Equatorial Current. Deep-Sea Res. 51, 209–228.
Christiansen, B., and A. Boetius (2000) Mass sedimentation of the swimming crab Charybdis smithii
(Crustacea: Decapoda) in the deep Arabian Sea. Deep-Sea Res. II. 47, 2673–2685.
Chung, S.P., et al. (1996) Beam attenuation and micro-organisms: spatial and temporal variations
in small particles along 140
W during the 1992 JGOFS EqPac transects. Deep-Sea Res. II. 43,
1205–1226.
Church, J.A. (1987) East Australian Current adjacent to the Great Barrier Reef. Aust. J. Mar.
Freshwat. Res. 38, 671–683.
Church, J.A., and P.D. Craig (1998) Australia’s shelf seas: diversity and complexity. In—The Sea,
Vol. 11, The Global Coastal Ocean (A.R. Robinson and K.H. Brink, Eds.), pp. 933–964. Wiley,
New York.
Church, J.A., et al. (1989) The Leeuwin Current. In—Poleward Flows along the Eastern Ocean
Boundaries (S.J. Neshyba, C.N.K. Mooers, R.L. Smith, and R.T. Barber, Eds.), pp. 230–253.
Springer-Verlag, New York.
Citeau, J., et al. (1988) The march of ITCZ migrations. Trop. Ocean-Atmos. Newslett. 45, 1–3.
Clark, P.U., et al. (2002) The role of the thermohaline circulation in abrupt climate change. Nature
(Lond.). 415, 863869.
Coachman, L.K. (1986) Circulation: water masses and fluxes on the southeastern Bering Sea shelf.
Cont. Shelf Res. 5, 22–108.
Coachman, L.K., et al. (1980) Frontal systems of the southeast Bering Sea shelf. In—Second International Symposium on Stratified Flows. Trondheim. June 1980 (T. Carstens and T. McClimans,
Eds.), pp. 917–933. 2
nd IAHR Symposium, Trondheim.
Coale, K.H et al. (1996a) Control of community growth and export production by upwelled iron
in the equatorial Pacific Ocean. Nature (Lond). 379, 621–624.
Coale, K.H., et al. (1996b) A massive phytoplankton bloom induced by an ecosystem-scale iron
fertilization experiment in the equatorial eastern Pacific Ocean. Nature (Lond.). 383, 495–501.
References
Chavez, F.P., et al. (1996) Phytoplankton variability in the central and eastern tropical Pacific.
Deep-Sea Res. II. 43, 835–870.
Chavez, F.P., et al. (2003) From anchovies to sardines and back: multidecadal change in the Pacific
Ocean. Science. 299, 217–221.
Chelton, D.B. (1982) Large-scale response of the California Current to forcing by the wind stress
curl. Rept. Calif. Coop. Fish. Invest. 23, 130–148.
Chelton, D.B., and M.G. Schlax (1996) Global observations of oceanic Rossby waves. Science. 272,
234–238.
Chelton, D.B., et al. (1982) Large-scale interannual physical and biological interaction in the
California Current. J. Mar. Res. 40, 1095–1125.
Chen, S., and B. Qiu (2004) Seasonal variability of the South Equatorial Countercurrent. J. Geophys.
Res. 109, C08003.
Chen, Y.-L. (2000) Comparisons of primary productivity and phytoplankton size structure in the
marginal regions of southern East China Sea. Cont. Shelf Res. 20, 437–458.
Chen, Y.-L., et al. (2001) New production in the East China Sea, comparison between well-mixed
winter and stratified summer conditions. Cont. Shelf Res. 21, 751–764.
Chen, Y.-L., et al. (2004) Phytoplankton production during a summer coastal upwelling in the East
China Sea. Cont. Shelf Res. 24, 1321–1338.
Chen, Z., et al. (1992) The effects of a Kuroshio frontal eddy on the biochemical structure of the
East China Sea. In—Essays on the Investigation of the Kuroshio 4, pp. 115–124. China Ocean
Press, Beijing.
Chester, R. (2000) Marine Chemistry—Trace Elements in the Ocean, p. 522. Blackwell, Oxford.
Childers, A.R., et al. (2005) Seasonal and interannual variability in the distribution of nutrients
and chlorophyll across the Gulf of Alaska shelf: 1998–2000. Deep-Sea Res. II. 52, 193–216.
Chisholm, S.W. (1992) Phytoplankton size. In—Primary Productivity and Biogeochemical Cycles in
the Sea (P. G. Falkowski and A. D. Woodhead, Eds.), pp. 213–237. Plenum Press, New York.
Chisholm, S.W., et al. (1988) A novel free-living prochlorophyte abundant in the oceanic photic
zone. Nature, Lond. 334, 340–343.
Christian J.R., et al. (2002) Biogeochemical modelling of the tropical Pacific Ocean. II. Iron
geochemistry. Deep-Sea Res. II. 49, 545–556.
Christian, J.R., et al. (2004) A ribbon of dark water: phytoplankton blooms in the meanders of the
Pacific North Equatorial Current. Deep-Sea Res. 51, 209–228.
Christiansen, B., and A. Boetius (2000) Mass sedimentation of the swimming crab Charybdis smithii
(Crustacea: Decapoda) in the deep Arabian Sea. Deep-Sea Res. II. 47, 2673–2685.
Chung, S.P., et al. (1996) Beam attenuation and micro-organisms: spatial and temporal variations
in small particles along 140
W during the 1992 JGOFS EqPac transects. Deep-Sea Res. II. 43,
1205–1226.
Church, J.A. (1987) East Australian Current adjacent to the Great Barrier Reef. Aust. J. Mar.
Freshwat. Res. 38, 671–683.
Church, J.A., and P.D. Craig (1998) Australia’s shelf seas: diversity and complexity. In—The Sea,
Vol. 11, The Global Coastal Ocean (A.R. Robinson and K.H. Brink, Eds.), pp. 933–964. Wiley,
New York.
Church, J.A., et al. (1989) The Leeuwin Current. In—Poleward Flows along the Eastern Ocean
Boundaries (S.J. Neshyba, C.N.K. Mooers, R.L. Smith, and R.T. Barber, Eds.), pp. 230–253.
Springer-Verlag, New York.
Citeau, J., et al. (1988) The march of ITCZ migrations. Trop. Ocean-Atmos. Newslett. 45, 1–3.
Clark, P.U., et al. (2002) The role of the thermohaline circulation in abrupt climate change. Nature
(Lond.). 415, 863869.
Coachman, L.K. (1986) Circulation: water masses and fluxes on the southeastern Bering Sea shelf.
Cont. Shelf Res. 5, 22–108.
Coachman, L.K., et al. (1980) Frontal systems of the southeast Bering Sea shelf. In—Second International Symposium on Stratified Flows. Trondheim. June 1980 (T. Carstens and T. McClimans,
Eds.), pp. 917–933. 2
nd IAHR Symposium, Trondheim.
Coale, K.H et al. (1996a) Control of community growth and export production by upwelled iron
in the equatorial Pacific Ocean. Nature (Lond). 379, 621–624.
Coale, K.H., et al. (1996b) A massive phytoplankton bloom induced by an ecosystem-scale iron
fertilization experiment in the equatorial eastern Pacific Ocean. Nature (Lond.). 383, 495–501.