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ATMOSPHERIC FORCING and its SPATIAL VARIABILITY
over the JAPAN/EAST SEA
Robert
Beardsley (WHOI)
Clive
Dorman (SDSU)
Richard
Limeburner (WHOI)
Alberto
Scotti (UNC)
January, 2001
Table of Contents
Winter circulation and water mass formation in the Japan/East Sea are thought to be strongly driven by surface wind stress and heat fluxes. Strong winds off Siberia during cold-air outbreaks and local topographic effects associated with the Sikhote-Alin mountain range that boarder the western rim of the Japan/East Sea may give rise to large spatially-concentrated surface stresses and associated heat and moisture fluxes which have direct and possibly large effects on the ocean.
Our primary objectives are 1) to determine the structure and variability of the MABL over the JES on synoptic and seasonal time scales, 2) to estimate surface wind stress and heat flux time series during summer and winter conditions, and 3) to examine the role of the coastal mountain ranges along the western perimeter of the JES on the low-level air flow and surface forcing during winter, with special emphasis on cold-air outbreak events that cause the maximum surface wind stresses and air-sea heat flux losses.
This project is part of the ONR Japan/East Sea Directed
Research Initiative to examine frontal processes, circulation, and water
property evolution in the Japan/East Sea during 1999-2000. The meterological
data collected in this project and modeling directly complements two other
components of the ONR JES program. C. Friehe and D. Khelif (UCI)
used an instrumented ONR Twin Otter aircraft to map the surface meteorological
fields and study the MABL structure over the central JES during late January-February
2000 (one flight overflew the Revelle). Flight patterns included
low-level (~ 30m) transects, with soundings to map the vertical structure
of the boundary layer. Some flights were timed to sample cold-air
outbreaks. S. Chen (UMiami) has collected both land-based and satellite
weather data in the JES region for 1999-2000 and used this data with global
weather model data to force a regional weather model and produce more highly
resolved surface weather fields for the study period.
Links to these two components are given below.
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Figure 1a |
Figure 1b |
Figure 2 |
Figure 3 |
Despite this past work, little is actually known about the marine boundary layer and surface forcing fields over the Japan/East Sea, especially during winter. We know of no modern profile measurements through the marine layer or moored measurements which allow accurate estimation of the surface heat flux components.
Theoretical, numerical, and laboratory investigations of flow past two-dimensional ridges and isolated circular and elliptical obstacles have demonstrated a rich array of dynamical flow structures including lee waves, hydraulic jumps, wakes, eddy generation and shedding, and upstream blocking and recirculation. Although the study of topographic effects in homogeneous and stratified flows is well-developed for idealized geometries, the role of the local orography in modifying and accelerating low-level winds during cold-air outbreaks in this region is unknown. The mountain ranges along the North Korean and Russian coasts reach heights of 1000m and higher, and are separated by an orographic gap at Vladivostok (Figure 1(a)). Manabe (1957) found that in this gap during one cold-air outbreak, the marine layer had a height of about 800m (with a strong inversion cap above), comparable to the height of the neighboring mountains. This suggests that the coastal mountains may effectively channel the cold dry Siberian air through the Vladivostok gap during cold-air outbreaks, causing strong spatial variability in the wind stress and surface heat flux over the JES. While there is some anecdotal evidence for this hypothesis, we know of no data collected to look at spatial variability in the surface forcing fields.
The basic surface measurements were made on the Revelle using the ship's IMET system and on the Khromov using WHOI self-contained ASIMET units. During the two Revelle SeaSoar cruises, two SDSU sensor sets were deployed on the bow mast below the IMET sensors, and one SDSU set near the top of the main mast, providing profile measurements over the maximum vertical sensor spacing available. The winter Revelle cruise featured additional IMET and ASIMET radiation sensors and J. Edson?s 3-axis sonic anemometer/thermometer/motion sensor system (Edson et at., 1998) mounted on the bow mast to allow direct covariance estimation of surface forcing during high wind cooling events.
Despite some IMET and ASIMET failures, the overall data return and data quality of the surface measurements were good. These data plus some additional data collected during the cruises should allow a full description of the surface meteorological conditions during the five cruises, plus bulk estimation of the surface wind stress during the five cruises and the surface heat and moisture fluxes on the two Revelle SeaSoar cruises and both Khromov cruises. Atmospheric soundings made on both Revelle SeaSoar cruises from the surface to above 10 km captured changes in the vertical structure of the MABL during synoptic shifts and winter cold-air outbreaks.
Table 1. JES cruises featuring meteorological measurements
collected by this component. The surface met data sets are considered "complete"
if accurate time series of wind velocity, air temperature, relative humidity,
pressure, incident short- and long-wave radiation, and SST can be constructed
using the best mix of IMET, ASIMET, SDSU, and other shipboard data.
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Figure 6. Schematic of air flow over coastal ranges
during a cold-air outbreak.
Dorman, C.E., S. M. Varlamov, and N.A. Dashko (2000). Cold Air Outbreaks over the Japan Sea During Winter 2000. ABSTRACT
Khelif,D., and C.A. Friehe (2000). Surface Forcing and Boundary-Layer Structure Over the Japan/East Sea During Winter Cold-Air Outbreaks. ABSTRACT
Lee, C.M., B.H. Jones, K.H. Brink, R. Arnone, R. Gould,
C. Dorman, R. Beardsley (2000). Upper Ocean Response to Cold Air Outbreaks
in the Japan/East Sea: SeaSoar Surveys at the Subpolar Front
ABSTRACT
Scotti, A. and R. Beardsley (2000). Hydraulically
Controlled Flow Across the Vladivostock Gap. ABSTRACT
Shipboard surface meteorological data:
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Also available via ftp
Carl Friehe (UCI)
Clive Dorman (SDSU)