 | National Assessment of Shoreline Change: Historical Shoreline Changes in the Hawaiian Islands By Charles H. Fletcher1, Bradley M. Romine1, Ayesha S. Genz1, Matthew M. Barbee1, Matthew Dyer1 405.23 Kb.  16 | read |
| National Assessment of Shoreline Change: Historical Shoreline Changes in the Hawaiian Islands By Charles H. Fletcher1, Bradley M. Romine1, Ayesha S. Genz1, Matthew M. Barbee1, Matthew Dyer1 208.65 Kb. 13 | read |
| National Assessment of Shoreline Change: Historical Shoreline Changes in the Hawaiian Islands By Charles H. Fletcher1, Bradley M. Romine1, Ayesha S. Genz1, Matthew M. Barbee1, Matthew Dyer1 209.31 Kb. 13 | read |
| National Assessment of Shoreline Change: Historical Shoreline Changes in the Hawaiian Islands By Charles H. Fletcher1, Bradley M. Romine1, Ayesha S. Genz1, Matthew M. Barbee1, Matthew Dyer1 209.83 Kb. 13 | 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 |
| M. A. Said+, M. A. Gerges, I. A. maiyza, M. A. Hussien and A. A. Radwan The paper investigates the changes in characteristics of the Atlantic Waters (AW) as they move eastwards along the Egyptian coast in the South-eastern Mediterranean 82.35 Kb. 1 | read |
| Dense waters of the Weddell and Scotia Seas: recent changes in properties and circulation Michael P. Meredith1,2, Loïc Jullion3,4, Peter J. Brown1,5, Alberto C. Naveira Garabato3 and Matthew P. Couldrey3 0.5 Mb. 3 | read |
| Precipitation from African Easterly Waves Itcz and its seasonal migration improves in the higher-resolution case. This suggests that capturing these transient waves and the resultant strong low-level convergence is one of the key ingredients for improving the simulation of precipitation in global 6.72 Mb. 4 | read |
| Delineation of the landward extent of wetlands and surface waters The methodology shall not be used to delineate areas which are not wetlands as defined in subsection 62-340. 200(19), F. A. C., nor to delineate as wetlands or surface waters areas exempted from delineation by statute or agency rule 0.61 Mb. 3 | read |
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