The effects of the island of Hawaii on offshore rainband evolution
The diurnal cycle of airflow on the island of Hawaii and the structure of the low-level flow separation line between the island-induced offshore flow and incoming trade winds are reasonably well understood. The formation and evolution of nocturnal and early morning rainfall on the windward side of t...
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| Veröffentlicht in: | Monthly weather review 2000-04, Vol.128 (4), p.1052-1069 |
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| container_title | Monthly weather review |
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| creator | WANG, J.-J RAUBER, R. M OCHS, H. T CARBONE, R. E |
| description | The diurnal cycle of airflow on the island of Hawaii and the structure of the low-level flow separation line between the island-induced offshore flow and incoming trade winds are reasonably well understood. The formation and evolution of nocturnal and early morning rainfall on the windward side of the island were found to be related to four major factors: (a) the existence or absence of trade wind cloud patches arriving from the northeast Pacific, (b) the effect of island blocking on the trade wind flow as it approaches the island, (c) the low-level convergence and thermal and moisture stratification near the flow separation line, and (d) the position of the flow separation line, controlled by both the Froude number and diabatic processes (nocturnal radiative cooling and evaporative cooling) occurring over the island. |
| doi_str_mv | 10.1175/1520-0493(2000)128<1052:teotio>2.0.co;2 |
| format | Article |
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The formation and evolution of nocturnal and early morning rainfall on the windward side of the island were found to be related to four major factors: (a) the existence or absence of trade wind cloud patches arriving from the northeast Pacific, (b) the effect of island blocking on the trade wind flow as it approaches the island, (c) the low-level convergence and thermal and moisture stratification near the flow separation line, and (d) the position of the flow separation line, controlled by both the Froude number and diabatic processes (nocturnal radiative cooling and evaporative cooling) occurring over the island.</abstract><cop>Boston, MA</cop><pub>American Meteorological Society</pub><doi>10.1175/1520-0493(2000)128<1052:teotio>2.0.co;2</doi><tpages>18</tpages><oa>free_for_read</oa></addata></record> |
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| source | American Meteorological Society; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Alma/SFX Local Collection |
| subjects | Aerodynamics Air flow Aircraft Convection, turbulence, diffusion. Boundary layer structure and dynamics Cooling Earth, ocean, space Exact sciences and technology External geophysics Flow separation Froude number Marine Meteorology Rain Studies Trade winds |
| title | The effects of the island of Hawaii on offshore rainband evolution |
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