70 likes | 164 Views
Findings from hindcast runs 04/30-05/21, 2002 Part II. List of runs. Week18-20 (04/30-05/21). Comparison of RUN1 and 3. Differences in the plume region are marginal. Some differences in the estuary; larger mixing length in the plume region leads to lower salinities in the estuary.
E N D
List of runs Week18-20 (04/30-05/21)
Comparison of RUN1 and 3 • Differences in the plume region are marginal. • Some differences in the estuary; larger mixing length in the plume region leads to lower salinities in the estuary.
Comparison between RUN1 and 2May 13, 2002 • Differences, although still non-trivial, are much smaller than previously observed. • Temperature comparison is not good as expected. (RUN[12]/CR2325_1205a.gif) • Salinity values are generally good; TSG shows RUN2 results are slightly better (RUN[12]/CR2325a_tsg_sal.gif). • This is mainly because of the cruise route being essentially east-west (RUN1/CR2325a_tsg_llgif). • There are some under-estimations of surface salinity in RUN2 (e.g., CR2325-1205a.gif), and over-estimation in RUN1 (e.g., CR2325-1223a.gif), which suggests plume is still somewhat skewed. • Towards end of this week, RUN1 elevations indicate certain instability which magnifies in week20, and may partly explain the large differences between the two results in that week. (COMP-RUN1-RUN2/nf2c5).
Comparison between RUN1 and 2May 15, 2002 • This is a better test for the model as the cruise route traverses a wider latitudes. (CR2327a_tsg_sal_map.gif) • For casts, RUN2 results capture better vertical profile (RUN[12]/CR2327_1107a.gif). • Cast locations are generally close to the mouth; had they been more away, the accuracy of RUN2 results might deteriorate. • For TSG, RUN1 results are slightly better (surprise!): • For this period, the wind is upwelling favorable, and plume should be moving southward; (RUN1/anim-sal_plume_min) • RUN2 results generally indicate a plume bent towards north. Cf. animations of plume at min.
Comparison between RUN1 and 2May 15, 2002 (cont’d) • However, RUN1 elevation doesn’t seem to be right; there is a large set-up in the plume and open-sea region (e.g. nf2c5). • This is believed to be the consequence of a larger minimum mixing length (3m) used. • As a result, the fresh water spreads faster towards the boundary and vertically downwards, creating larger baroclinic velocity. (RUN1/anim-sal_far_min.gif) • Results indicate the direction in which plume is moving is still not right with the refinement, especially for upwelling favorable winds. (RUN2/anim-sal_far_min.gif)
Future work • Since raising the minimum mixing length (xl) didn’t seem to make much difference except creating instability, we’d run the refined grid with original xl (2m).