506
References
Mulhearn, P.J. (1987) The Tasman front: a study using satellite infrared imagery. J. Phys.
Oceanogr. 17, 1148–1155.
Müller, P., and C. Garrett (2002) From stirring to mixing in a stratified ocean. Oceanography 15,
12–19.
Müller-Karger, F.E., et al. (1988) The dispersal of the Amazon’s water. Nature (Lond.). 333, 56–59.
Müller-Karger, F.E., et al. (1989) Pigment observations in the Caribbean Sea: observations from
space. Prog. Oceanogr. 35, 23–64.
Muller-Karger, F.E., et al. (2004) Processes of coastal upwelling and carbon flux in the Carioco
Basin. Deep-Sea Res. II. 51, 927–943.
Murphy, R.J., et al. (2001) Phytoplankton distributions around New Zealand derived from SeaWiFS
remotely-sensed ocean colour data. N. Z. J. Mar. Freshwat. Res. 35, 343–362.
Murray, J.W., et al. (1995) A US JGOFS Process Study in the equatorial Pacific (EqPac). Deep-Sea
Res. II. 42, 275–293.
Murray, J.W., and E. Izdar (1989) The 1988 Black Sea oceanographic expedition: overview and
new discoveries. Oceanography. 2, 15–21.
Murray, J.W., Ed. (1991) Black Sea oceanography. Deep-Sea Res. 38(Suppl. 2A), S655–S1266
Nagata, H.S.O. (1998) Seasonal changes and vertical distributions of chlorophyll and primary
productivity on the Yamato Rise, central Japan Sea. Plankt. Biol. Ecol. 45, 159–170.
Nagata, Y., et al. (1986) Detailed structure of the Kuroshio Front and the origin of the water in
warm-core rings. Deep-Sea Res. 33, 1509–1526.
Nair, S.R., et al. (1981) Zooplankton composition and diversity in western Bay of Bengal. J. Plankton
Res. 3, 493–508.
Naqui S.W.A., et al. (2000) Increased marine production of N 2 O due to intensifying anoxia on the
Indian continental shelf. Nature (Lond.). 408, 346–349.
Nathansohn, A. (1909) Beiträge zur Biologie des Planktons. II. Vertikalzirkulation und Planktonmaxima im Mittelmeer. Int. Rev. Ges. Hydrobiol. 2, 580–632.
Nelson D.M., and W.O. Smith (1991) Sverdrup re-visited: critical depths, maximum chlorophyll
levels and the control of the Southern Ocean productivity by the irradiance-mixing regime.
Limnol. Oceanogr. 36, 1650–1661.
Nelson, D.M., et al. (2001) A seasonal progression of Si limitation in the Pacific sector of the
Southern Ocean. Deep-Sea Res. II. 48, 3973–3995.
Nelson, D.M., et al. (2002) Vertical budgets for organic carbon and biogenic silica in the Pacific
sector of the Southern Ocean, 1996–1998. Deep-Sea Res. II. 49, 1645–1674.
Nelson, G., and L. Hutchings (1983) The Benguela upwelling area. Prog. Oceanogr. 12, 333–356.
Nelson, N.B., et al. (2004) The spring bloom in the NW Sargasso Sea: spatial extent and relationship
with winter mixing. Deep-Sea Res. II. 51, 987–1000.
Nemoto, T., and W.G. Harrison (1981) High latitude ecosystems. In—Analysis of Marine Ecosystems
(A.R. Longhurst, Ed.), pp. 95–126. Academic Press, London.
Neumann, G. (1969) The Equatorial Undercurrent in the Atlantic Ocean. Proc. Symp. Oceanogr.
Fish. Res. Trop. Atlantic UNESCO, 33–44.
Newell, B.S. (1959) The hydrography of British East African coastal waters. Col. Off. Fish. Pubs.
Lond. 12, 1–118.
Niemann, H., et al. (2004) Red Sea gravity currents cascade near-reef phytoplankton to the twilight
zone. Mar. Ecol. Prog. Ser. 269, 91–99.
Niemann, R.G. (2003) The interplay between upwelling and deep convective mixing in the Gulf of
Aqaba. Limnol. Oceanogr. 48, 2355–2368.
Niermann, U. (1986) Distribution of Sargassum natans and some of its epibionts in the Sargasso
Sea. Helgol. Meeresunters. 40, 343–353.
Niiler, P.P. (1977) One-dimensional models of the seasonal thermocline. In—The Sea
(E.D. Goldberg, Ed.), pp. 97–115. Wiley, New York.
Nishikawa, T., et al. (2000) Effects of temperature and salinity on the growth of the giant diatom
Coscinodiscus wailesii isolated from Harima-Nada, Seto Inland Sea. Nipp. Suis. Gak. 66, 993–998.
Nitani, H. (1972) The beginning of the Kuroshio. In—Kuroshio: Physical Aspects of the Japan
Current (H. Stommel and K. Yoshida, Eds.), pp. 129–164. University of Washington Press,
Seattle, WA.
Nittrouer, C.A., and D.J. DeMaster (1996) The Amazon shelf setting: tropical, energetic and
influenced by a large river. Cont. Shelf Res. 16, 553–573.
References
Mulhearn, P.J. (1987) The Tasman front: a study using satellite infrared imagery. J. Phys.
Oceanogr. 17, 1148–1155.
Müller, P., and C. Garrett (2002) From stirring to mixing in a stratified ocean. Oceanography 15,
12–19.
Müller-Karger, F.E., et al. (1988) The dispersal of the Amazon’s water. Nature (Lond.). 333, 56–59.
Müller-Karger, F.E., et al. (1989) Pigment observations in the Caribbean Sea: observations from
space. Prog. Oceanogr. 35, 23–64.
Muller-Karger, F.E., et al. (2004) Processes of coastal upwelling and carbon flux in the Carioco
Basin. Deep-Sea Res. II. 51, 927–943.
Murphy, R.J., et al. (2001) Phytoplankton distributions around New Zealand derived from SeaWiFS
remotely-sensed ocean colour data. N. Z. J. Mar. Freshwat. Res. 35, 343–362.
Murray, J.W., et al. (1995) A US JGOFS Process Study in the equatorial Pacific (EqPac). Deep-Sea
Res. II. 42, 275–293.
Murray, J.W., and E. Izdar (1989) The 1988 Black Sea oceanographic expedition: overview and
new discoveries. Oceanography. 2, 15–21.
Murray, J.W., Ed. (1991) Black Sea oceanography. Deep-Sea Res. 38(Suppl. 2A), S655–S1266
Nagata, H.S.O. (1998) Seasonal changes and vertical distributions of chlorophyll and primary
productivity on the Yamato Rise, central Japan Sea. Plankt. Biol. Ecol. 45, 159–170.
Nagata, Y., et al. (1986) Detailed structure of the Kuroshio Front and the origin of the water in
warm-core rings. Deep-Sea Res. 33, 1509–1526.
Nair, S.R., et al. (1981) Zooplankton composition and diversity in western Bay of Bengal. J. Plankton
Res. 3, 493–508.
Naqui S.W.A., et al. (2000) Increased marine production of N 2 O due to intensifying anoxia on the
Indian continental shelf. Nature (Lond.). 408, 346–349.
Nathansohn, A. (1909) Beiträge zur Biologie des Planktons. II. Vertikalzirkulation und Planktonmaxima im Mittelmeer. Int. Rev. Ges. Hydrobiol. 2, 580–632.
Nelson D.M., and W.O. Smith (1991) Sverdrup re-visited: critical depths, maximum chlorophyll
levels and the control of the Southern Ocean productivity by the irradiance-mixing regime.
Limnol. Oceanogr. 36, 1650–1661.
Nelson, D.M., et al. (2001) A seasonal progression of Si limitation in the Pacific sector of the
Southern Ocean. Deep-Sea Res. II. 48, 3973–3995.
Nelson, D.M., et al. (2002) Vertical budgets for organic carbon and biogenic silica in the Pacific
sector of the Southern Ocean, 1996–1998. Deep-Sea Res. II. 49, 1645–1674.
Nelson, G., and L. Hutchings (1983) The Benguela upwelling area. Prog. Oceanogr. 12, 333–356.
Nelson, N.B., et al. (2004) The spring bloom in the NW Sargasso Sea: spatial extent and relationship
with winter mixing. Deep-Sea Res. II. 51, 987–1000.
Nemoto, T., and W.G. Harrison (1981) High latitude ecosystems. In—Analysis of Marine Ecosystems
(A.R. Longhurst, Ed.), pp. 95–126. Academic Press, London.
Neumann, G. (1969) The Equatorial Undercurrent in the Atlantic Ocean. Proc. Symp. Oceanogr.
Fish. Res. Trop. Atlantic UNESCO, 33–44.
Newell, B.S. (1959) The hydrography of British East African coastal waters. Col. Off. Fish. Pubs.
Lond. 12, 1–118.
Niemann, H., et al. (2004) Red Sea gravity currents cascade near-reef phytoplankton to the twilight
zone. Mar. Ecol. Prog. Ser. 269, 91–99.
Niemann, R.G. (2003) The interplay between upwelling and deep convective mixing in the Gulf of
Aqaba. Limnol. Oceanogr. 48, 2355–2368.
Niermann, U. (1986) Distribution of Sargassum natans and some of its epibionts in the Sargasso
Sea. Helgol. Meeresunters. 40, 343–353.
Niiler, P.P. (1977) One-dimensional models of the seasonal thermocline. In—The Sea
(E.D. Goldberg, Ed.), pp. 97–115. Wiley, New York.
Nishikawa, T., et al. (2000) Effects of temperature and salinity on the growth of the giant diatom
Coscinodiscus wailesii isolated from Harima-Nada, Seto Inland Sea. Nipp. Suis. Gak. 66, 993–998.
Nitani, H. (1972) The beginning of the Kuroshio. In—Kuroshio: Physical Aspects of the Japan
Current (H. Stommel and K. Yoshida, Eds.), pp. 129–164. University of Washington Press,
Seattle, WA.
Nittrouer, C.A., and D.J. DeMaster (1996) The Amazon shelf setting: tropical, energetic and
influenced by a large river. Cont. Shelf Res. 16, 553–573.