Killworth, P. D., 1995: Hydraulic control and maximal flow in rotating, stratified hydraulics. DeepSea Res. 42, 859–871. [5.6]
Killworth, P. D., 1997: On the parameterization of
eddy transfer. Part I: Theory. J. Mar. Res. 55,
1171–1197. [5.2, 7.2]
Killworth, P. D. and N. R. Edwards, 1999: A turbulent bottom boundary layer code for use in
numerical ocean models. J. Phys. Oceanogr. 29,
1221–1238. [2.2, 2.3]
Killworth, P. D. and M. M. Nanneh, 1994: Isopycnal
momentum budget of the Antarctic Circumpolar Current in the Fine Resolution Antarctic
Model. J. Phys. Oceanogr., 24, 1201–1223.
[4.6]
Killworth, P. D., D. Stainforth, D. J. Webb and S. M.
Paterson, 1991: The development of a free surface
Bryan-Cox-Semtner ocean model. J. Phys.
Oceanogr. 21, 1333–1348. [2.3]
Killworth, P. D., D. B. Chelton and R. A. De Szoeke,
1997: The speed of observed and theoretical long
extra-tropical planetary waves. J. Phys. Oceanogr.
27, 1946–1966. [3.3, 7.1]
Killworth, P. D., D. A. Smeed and A. J . G. Nurser,
2000: The effects on ocean models of relaxation
towards observations at the surface. J. Phys.
Oceanogr. 30, 160–174. [5.1]
Kinder, T. H. and G. Parrilla, 1987: Yes, some of the
Mediterranean outflow does come from great
depth. J. Geophys. Res. 92, 2901–2906. [5.7]
Kindle, J. C. and J. D. Thompson, 1989: The 26and 50-day oscillations in the western Indian
Ocean: model results. J. Geophys. Res. 94, 4721–
4736. [3.3]
Kindle, J. C., H. E. Hurlburt and E. J. Metzger, 1989:
On the seasonal and interannual variability of
the Pacific–Indian Ocean throughflow. Western
Pacific International Meeting and Workshop
on TOGA-COARE, J. Picaut, R. Lukas and
T. Delcroix (eds), Noumea, New Caledonia,
pp. 355–366. [4.7]
King, B. A. and S. G. Alderson, 1994: SR1 repeat
hydrography/ADCP, Drake Passage, November
1993. International WOCE Newsletter, No. 15,
13–15, WOCE International Project Office
(unpublished document). [3.1]
King, B. A. and E. B. Cooper, 1993: Comparison of
ships heading determined from an array of GPS
antennas with heading from conventional gyrocompass measurements. Deep-Sea Res. 40, 2207–
2216. [3.1]
King, B. A., S. G. Alderson and D. Cromwell, 1996:
Enhancement of shipboard ADCP data with
DGPS position and GPS heading measurements.
Deep-Sea Res. 43, 937–947. [3.1]
Kitamura, Y. and N. Suginohara, 1987: Effect of
vertical viscosity and diffusivity on tropical ocean
circulation: subsurface eastward flow. J.
Oceanogr. Soc. Japan 43, 1–20. [4.3]
Kitani, K., 1973: An oceanographic study of the
Okhotsk Sea – particularly in regard to cold waters.
Bull. Far Seas Fish. Res. Lab. 9, 45–77. [5.4]
Kitoh, A., 1991: Interannual variations in an atmospheric GCM forced by the 1970–1989 SST Part II:
low frequency variability of the wintertime
Northern Hemisphere extratropics. J. Meteor. Soc.
Japan 69, 271–291. [7.3]
Kleeman, R., A. M. Moore and N. R. Smith, 1995:
Assimilation of sub-surface thermal data into an
intermediate tropical coupled ocean–atmosphere
model. Mon. Wea. Rev. 123, 3103–3113. [7.4]
Kleeman, R., R. Colman, N. R. Smith and S. B. Power,
1996: A recent change in the mean state of the
Pacific Ocean: Observational evidence and atmospheric and oceanic responses. J. Geophys. Res. 101,
20483–20500. [7.4]
Kleeman, R., J. P. McCreary and B. A. Klinger, 1999:
A mechanism for generating ENSO decadal
variability. Geophys. Res. Lett. 26, 1743–1746.
[5.3]
Klein, B., R. L. Molinari, T. J. Müller and G. Siedler,
1995: A transatlantic section at 14.5°N: Meridional
volume and heat fluxes. J. Mar. Res. 53, 929–
957. [6.1]
Klein, B. and N. Hogg, 1996: On the variability of
18 Degree Water formation as observed from
moored instruments at 55°W. Deep-Sea Res. 43,
1777–1806. [5.4]
Klinck, J. M., 1993: Effects of wind, density, and
bathymetry on a one-layer Southern Ocean model.
J. Geophys. Res. 97, 20179–20189. [4.6]
Knapp, G. P., 1988: Hydrographic Data from
R. V. Endeavor Cruise 129. Woods Hole Oceanographic Institution, Technical Report, WHOI88-41, 111 pp. [7.3]
Knox, R. A., 1976: On a long series of measurements
of Indian Ocean equatorial currents near Addu
Atoll. Deep-Sea Res. 23, 211–221. [4.3]
Knudsen, M., 1900: Ein hydrographische Lehrsatz.
Analen der Hydrographie und Marinen Meteorologie 28, 316–320. [7.4]
Knudsen, M. (ed.), 1901: Hydrographical Tables.
G. E . C. Gad, Copenhagen, 63 pp. [7.4]
Knutson, T. R. and S. Manabe, 1998: Model assessment of decadal variability and trends in the tropical Pacific Ocean. J. Climate 11, 2273–2296. [2.3]
Knutson, T. R., S. Manabe and D. Gu, 1997:
Simulated ENSO in a global coupled ocean–atmosphere model: Multidecadal amplitude modulation
and CO 2 sensitivity. J. Climate 10, 42–63. [2.3]
REFERENCES
637
Killworth, P. D., 1997: On the parameterization of
eddy transfer. Part I: Theory. J. Mar. Res. 55,
1171–1197. [5.2, 7.2]
Killworth, P. D. and N. R. Edwards, 1999: A turbulent bottom boundary layer code for use in
numerical ocean models. J. Phys. Oceanogr. 29,
1221–1238. [2.2, 2.3]
Killworth, P. D. and M. M. Nanneh, 1994: Isopycnal
momentum budget of the Antarctic Circumpolar Current in the Fine Resolution Antarctic
Model. J. Phys. Oceanogr., 24, 1201–1223.
[4.6]
Killworth, P. D., D. Stainforth, D. J. Webb and S. M.
Paterson, 1991: The development of a free surface
Bryan-Cox-Semtner ocean model. J. Phys.
Oceanogr. 21, 1333–1348. [2.3]
Killworth, P. D., D. B. Chelton and R. A. De Szoeke,
1997: The speed of observed and theoretical long
extra-tropical planetary waves. J. Phys. Oceanogr.
27, 1946–1966. [3.3, 7.1]
Killworth, P. D., D. A. Smeed and A. J . G. Nurser,
2000: The effects on ocean models of relaxation
towards observations at the surface. J. Phys.
Oceanogr. 30, 160–174. [5.1]
Kinder, T. H. and G. Parrilla, 1987: Yes, some of the
Mediterranean outflow does come from great
depth. J. Geophys. Res. 92, 2901–2906. [5.7]
Kindle, J. C. and J. D. Thompson, 1989: The 26and 50-day oscillations in the western Indian
Ocean: model results. J. Geophys. Res. 94, 4721–
4736. [3.3]
Kindle, J. C., H. E. Hurlburt and E. J. Metzger, 1989:
On the seasonal and interannual variability of
the Pacific–Indian Ocean throughflow. Western
Pacific International Meeting and Workshop
on TOGA-COARE, J. Picaut, R. Lukas and
T. Delcroix (eds), Noumea, New Caledonia,
pp. 355–366. [4.7]
King, B. A. and S. G. Alderson, 1994: SR1 repeat
hydrography/ADCP, Drake Passage, November
1993. International WOCE Newsletter, No. 15,
13–15, WOCE International Project Office
(unpublished document). [3.1]
King, B. A. and E. B. Cooper, 1993: Comparison of
ships heading determined from an array of GPS
antennas with heading from conventional gyrocompass measurements. Deep-Sea Res. 40, 2207–
2216. [3.1]
King, B. A., S. G. Alderson and D. Cromwell, 1996:
Enhancement of shipboard ADCP data with
DGPS position and GPS heading measurements.
Deep-Sea Res. 43, 937–947. [3.1]
Kitamura, Y. and N. Suginohara, 1987: Effect of
vertical viscosity and diffusivity on tropical ocean
circulation: subsurface eastward flow. J.
Oceanogr. Soc. Japan 43, 1–20. [4.3]
Kitani, K., 1973: An oceanographic study of the
Okhotsk Sea – particularly in regard to cold waters.
Bull. Far Seas Fish. Res. Lab. 9, 45–77. [5.4]
Kitoh, A., 1991: Interannual variations in an atmospheric GCM forced by the 1970–1989 SST Part II:
low frequency variability of the wintertime
Northern Hemisphere extratropics. J. Meteor. Soc.
Japan 69, 271–291. [7.3]
Kleeman, R., A. M. Moore and N. R. Smith, 1995:
Assimilation of sub-surface thermal data into an
intermediate tropical coupled ocean–atmosphere
model. Mon. Wea. Rev. 123, 3103–3113. [7.4]
Kleeman, R., R. Colman, N. R. Smith and S. B. Power,
1996: A recent change in the mean state of the
Pacific Ocean: Observational evidence and atmospheric and oceanic responses. J. Geophys. Res. 101,
20483–20500. [7.4]
Kleeman, R., J. P. McCreary and B. A. Klinger, 1999:
A mechanism for generating ENSO decadal
variability. Geophys. Res. Lett. 26, 1743–1746.
[5.3]
Klein, B., R. L. Molinari, T. J. Müller and G. Siedler,
1995: A transatlantic section at 14.5°N: Meridional
volume and heat fluxes. J. Mar. Res. 53, 929–
957. [6.1]
Klein, B. and N. Hogg, 1996: On the variability of
18 Degree Water formation as observed from
moored instruments at 55°W. Deep-Sea Res. 43,
1777–1806. [5.4]
Klinck, J. M., 1993: Effects of wind, density, and
bathymetry on a one-layer Southern Ocean model.
J. Geophys. Res. 97, 20179–20189. [4.6]
Knapp, G. P., 1988: Hydrographic Data from
R. V. Endeavor Cruise 129. Woods Hole Oceanographic Institution, Technical Report, WHOI88-41, 111 pp. [7.3]
Knox, R. A., 1976: On a long series of measurements
of Indian Ocean equatorial currents near Addu
Atoll. Deep-Sea Res. 23, 211–221. [4.3]
Knudsen, M., 1900: Ein hydrographische Lehrsatz.
Analen der Hydrographie und Marinen Meteorologie 28, 316–320. [7.4]
Knudsen, M. (ed.), 1901: Hydrographical Tables.
G. E . C. Gad, Copenhagen, 63 pp. [7.4]
Knutson, T. R. and S. Manabe, 1998: Model assessment of decadal variability and trends in the tropical Pacific Ocean. J. Climate 11, 2273–2296. [2.3]
Knutson, T. R., S. Manabe and D. Gu, 1997:
Simulated ENSO in a global coupled ocean–atmosphere model: Multidecadal amplitude modulation
and CO 2 sensitivity. J. Climate 10, 42–63. [2.3]
REFERENCES
637