Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Steven H. Boyd"'
Publikováno v:
Deep Sea Research Part A. Oceanographic Research Papers. 39:S247-S278
A 1-m 2 MOCNESS with 20 nets was used to make a series of tows in Gulf Stream meander/ring 82-H (September/October 1982) including two 0–100 m undulating “towyos”. One towyo, made at dusk in the core of 82-H (of Sargasso Sea/Gulf Stream origin)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::28fc113f0a569d2b1ac54c7914425b27
https://doi.org/10.1016/s0198-0149(11)80015-4
https://doi.org/10.1016/s0198-0149(11)80015-4
Autor:
Steven H. Boyd, Edward M. Hulburt, Peter B. Ortner, Edward J. Carpenter, James L. Cox, George P. Knapp, Peter H. Wiebe, Andrew E. Jahn
Publikováno v:
Deep Sea Research and Oceanographic Abstracts. 23:695-710
Gulf Stream cold core rings are major oceanographic features in the northwestern Atlantic Ocean. During formation, cold water of Slope origin and the associated flora and fauna are entrapped within a ring of Gulf Stream water. These systems generally
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0609a653503f755425feabc342ccc3ab
https://doi.org/10.1016/s0011-7471(76)80015-0
https://doi.org/10.1016/s0011-7471(76)80015-0
Publikováno v:
Deep Sea Research and Oceanographic Abstracts. 23:1217-1229
Field studies and tow basin experiments of Longhurst-Hardy Plankton Recorder (LHPR) biases were conducted by injecting various types of particles into an LHPR having a variety of net and recorder box configurations. Tow speed and clogging were also c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba1e2239df090ad45911918d838cfa0b
https://doi.org/10.1016/0011-7471(76)90899-8
https://doi.org/10.1016/0011-7471(76)90899-8
Autor:
Steven H. Boyd
Publikováno v:
Physiological Zoology. 48:225-234
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bbe631e96709002a8087ccffd71ba0f6
https://doi.org/10.1086/physzool.48.3.30160944
https://doi.org/10.1086/physzool.48.3.30160944
Publikováno v:
Deep Sea Research Part A. Oceanographic Research Papers. 33:1885-1905
Micronekton biomass was sampled in warm-core Gulf Stream ring 82-B (at ages 2, 4 and 6 months), the Slope Water, the Gulf Stream and the Sargasso Sea during three multi-ship cruises. There was no significant diel difference in the 0–1000 m integrat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::13a906e1b94e4c98b514119f68e96900
https://doi.org/10.1016/0198-0149(86)90084-1
https://doi.org/10.1016/0198-0149(86)90084-1
Publikováno v:
Limits of Nematoscelis megalops in the northwestern Atlantic in relation to Gulf Stream cold core rings. II, Physiological and biochemical effects of expatriation
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0467d432311012d62ad788c9ddfe5553
https://doi.org/10.1575/1912/6977
https://doi.org/10.1575/1912/6977
Autor:
Steven H. Boyd, Peter H. Wiebe
Publikováno v:
Limits of Nematoscelis megalops in the northwestern Atlantic in relation to Gulf Stream cold core rings. I, Horizontal and vertical distributions
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3667b3f951e13510c06e673acbb66e61
https://doi.org/10.1575/1912/6978
https://doi.org/10.1575/1912/6978
Publikováno v:
Particulate matter sinking to the deep-sea floor at 2000 M in the Tongue of the Ocean, Bahamas, with a description of a new sedimentation trap
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f2171b0b29a2935866f33578f4734ba4
https://doi.org/10.1575/1912/1792
https://doi.org/10.1575/1912/1792
Publikováno v:
Journal of Geophysical Research. 90:8885
The vertical and horizontal distribution of macrozooplankton biomass was measured at four time points in warm-core ring 82B. Samples were also collected in two other warm-core rings, the Slope Water, nine cold-core rings, and the Sargasso Sea. Biomas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cb1ba8d5bf5efb915d3ce112340323c6
https://doi.org/10.1029/jc090ic05p08885
https://doi.org/10.1029/jc090ic05p08885