A Numerical Study of the Effect of the Gulf Stream and the Appalachian Mountains on Carolina Coastal Frontogenesis

Three numerical experiments were conducted to understand the role of the Gulf Stream and the Appalachian mountains on the formation of coastal frontogenesis along the mid-Atlantic coast during the winter months. A 3-dimensional, 10-layer, 1-way interactive, triple-nested hydrostatic model was used....

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Bibliographic Details
Main Authors: Xu, Liang, Raman, Sethu, Madala, Rangarao V.
Other Authors: NAVAL RESEARCH LAB WASHINGTON DC
Format: Text
Language:English
Published: 1995
Subjects:
Physical and Dynamic Oceanography
Atmospheric Physics
*COASTAL REGIONS
*GULF STREAM
*FRONTS(OCEANOGRAPHY)
*APPALACHIAN MOUNTAINS
HEAT TRANSFER
MATHEMATICAL MODELS
COMPUTERIZED SIMULATION
LOW TEMPERATURE
EXPERIMENTAL DATA
OCEAN CURRENTS
AIR FLOW
BOUNDARY LAYER
OCEANOGRAPHIC DATA
WINTER
ATMOSPHERIC PRECIPITATION
NUMERICAL METHODS AND PROCEDURES
ATLANTIC OCEAN
AIR WATER INTERACTIONS
HEAT FLUX
ARCTIC REGIONS
CONVECTION(ATMOSPHERIC)
AIR MASSES
PE61153N
Arctic
Raleigh
Online Access:http://www.dtic.mil/docs/citations/ADA293765
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA293765
Description
Summary:Three numerical experiments were conducted to understand the role of the Gulf Stream and the Appalachian mountains on the formation of coastal frontogenesis along the mid-Atlantic coast during the winter months. A 3-dimensional, 10-layer, 1-way interactive, triple-nested hydrostatic model was used. The model physics includes dry convective adjustment, explicit large-scale precipitation, parameterized convective-scale circulations, and parameterized boundary layer physics using a similarity theory formulation. Initial conditions for the numerical model are obtained from the Second intensive Observation Period (IOP-2) of the Genesis of Atlantic Lows Experiment (GALE). Results of the numerical experiments show that the Gulf Stream plays a significant role in developing coastal frontogenesis through transfer of large amounts of sensible and latent heats to the cold, dry atmospheric air of Arctic origin. The Gulf Stream is also found to be crucial in producing convective precipitation along the Carolina coast. On the other hand, the Appalachian mountains, which are responsible for cold air damming, are found to play only a minor role in the coastal frontogenesis. (AN) Prepared in collaboration with North Carolina State Univ., Raleigh, Dept. of Marine, Earth, and Atmospheric Sciences.

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