Accession Number : ADA330922
Title : The Influence of Mesoscale Orography on a Coastal Jet and Rainband.
Descriptive Note : Rept. for 1 Apr-31 Dec 96,
Corporate Author : NAVAL RESEARCH LAB MONTEREY CA
Personal Author(s) : Doyle, James D.
PDF Url : ADA330922
Report Date : 24 OCT 1996
Pagination or Media Count : 61
Abstract : The role of mesoscale orography along the central California coast in the development and evolution of a coastal jet and rainband is investigated using a high-resolution, triply- nested, nonhydrostatic numerical model. Comparison of the model simulations, which use horizontal grid increments of 5 km and 2 km on the inner-computational meshes, with a coastal mesoscale observation network indicates that the fine-scale structure of the jet and rainband dynamics are adequately simulated, although phase and orientation errors occur. The observed and simulated near-surface winds have maximum speeds that exceed 22 m/s and a direction nearly parallel to the coastline and topography. Force balance analysis indicates that blocking in the lowest 500 m and flow over the coastal range above this layer contribute to mesoscale pressure perturbations, including pressure ridging upstream of the coastal mountains, which force the ageostrophic dynamics of the coastal jet. Pressure perturbations associated with the topographic flows induce a complex mesoscale response that adds rich mesoscale structure to the jet including a wake region that forms on the lee side of the coastal range that limits the horizontal scale of the jet. Sensitivity test results underscore the multi-process character of the coastal dynamics, and the importance of the coastal topography and diiferential frictional drag at the land/sea interface for the formation and amplification of the jet. The mesoscale response to steep coastal topography results in a 45% enhancement to the near-surface jet strength. The onshore movement of line convection at the leading edge of a weak front is impeded by steep coastal topography in both the radar observations and numerical simulations. Low-level blocking forces the rainband to emulate a wedge-shaped structure with a coastal jet that is dynamically trapped between the steep
Descriptors : *RAINFALL, *COLD FRONTS, COMPUTERIZED SIMULATION, COASTAL REGIONS, WIND, NUMERICAL ANALYSIS, RADAR, TOPOGRAPHY, PERTURBATIONS, CALIFORNIA, CONVECTION(HEAT TRANSFER), OROGRAPHY.
Subject Categories : Meteorology
Distribution Statement : APPROVED FOR PUBLIC RELEASE