 | The origin of along-shelf pressure gradient in the Middle Atlantic Bight Mab, and they produce sea surface sloping down to the north when they move further south. The influence of large-scale wind pattern on aspg is also examined 57.55 Kb.  1 | read |
| The origin of along-shelf pressure gradient in the Middle Atlantic Bight Cape Hatteras. It is shown that the large-scale wind pattern cannot directly affect the aspg. However, north of the Gulf Stream, there exist seasonal and inter-annual variations of eddy kinetic energy which affect the aspg 53.97 Kb. 1 | read |
| The origin of along-shelf pressure gradient in the Middle Atlantic Bight Cape Hatteras. It is also shown that the large-scale wind cannot directly affect the aspg. However, north of the Gulf Stream, there exist seasonal and inter-annual variations of eddy kinetic energy which affect the aspg 134.95 Kb. 2 | read |
| The origin of along-shelf pressure gradient in the Middle Atlantic Bight Cape Hatteras. It is shown that the large-scale wind pattern cannot directly affect the aspg. On the other hand, north of the Gulf Stream, there exist seasonal and inter-annual variations of eddy kinetic energy which affect the aspg 74.87 Kb. 1 | read |
| Through the hindenburg line to cambrai C. in-C. told him forcibly that every effort should be made to get a decision in the present autumn. The Germans were being outlasted and beaten 143.88 Kb. 4 | read |
| T jpo, 2011, in press he origin of along-shelf pressure gradient in the Middle Atlantic Bight Coastal Labrador Sea Water (clsw) transport contribute to a positive mean aspg (tilt up northward) approximately in the ratio 1: 7 (I e. Clsw dominates), whereas wind and Gulf Stream tend to produce a negative mean aspg, approximately 1: 6 1.87 Mb. 13 | read |
| Decadal Ventilation and Mixing of Indian Ocean Waters rana a. Fine Rana a. Finea*, william m. Smethie, jrb, john L. Bullisterc, monika rheind, dong-ha mine, mark j. Warnerf, alain poissong, and ray f. Weissh 87.51 Kb. 1 | read |
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