[Eoas-seminar] COAPS Short Seminar Series - Monday Sept. 12th at 11:00AM - revised
eoas-seminar at lists.fsu.edu
eoas-seminar at lists.fsu.edu
Mon Sep 12 09:44:26 EDT 2022
These talks are usually scheduled for the first Monday of each month.
The first talk normally starts at 11:00AM. Each talk is typically 12
minutes long (similar to many professional meetings), with 8 minutes for
questions.
These talks will be presented via Zoom, with the following connection
information:
https://fsu.zoom.us/j/98491660566?pwd=NzBxNzN4LzdsbSs4R3B6RzliOGhhdz09
Meeting ID: 984 9166 0566
Passcode: 478314
Sept. 12th:
Xu Chen: Modeling the transport of oyster larvae from spawning areas to
suitable juvenile habitat (settlement zones) in Apalachicola Bay, Florida
Description: Based on an offline Lagrangian model (FISCM), an oyster
larvae model was developed to study the transport of oyster larvae from
spawning areas to suitable juvenile habitat (settlement zones) in
Apalachicola Bay, Florida. Velocity fields from FVCOM outputs were used
to drive the Lagrangian advection. The vertical random walk proposed by
Visser (1997) is used for calculating the effect of vertical
diffusivity. In this experiment, more than 1 million Lagrangian floats
were released between May 1 and May 31, 2012, at the frequency of 10504
floats per 6 hours and the simulation ran for 50 days. These floats are
released at oyster habitat sites in Apalachicola Bay, Alligator Harbor,
and Ochlockonee Bay. In this model, one float represents a group of
oyster larvae, and 100% of the larvae in the group are considered alive
when the float is released. If this larvae group is surrounded by
salinity between 6 ppt and 27 ppt and temperature between 5 oC and
32 oC, the percentage of alive larvae will not change. However, if the
float is surrounded by water out of the normal ranges of salinity and
temperature as depicted above, 95% of the larvae in the group will die
in 1 week. Each float (oyster larvae group) has a liberty period of 20
days before settling, and a successful settling can be achieved only
when the float meets more than one oyster habitat region. This talk will
present some preliminary results of the oyster larvae model.
Ethan Wright: A Comparison of Scatterometer Wind Derivative Calculation
Methods
Description: Spatial wind derivatives, such as vorticity and divergence,
are important variables used to characterize low-level atmospheric flow
and spatial derivatives of wind stress are fundamentally important for
ocean forcing. Scatterometer swath winds are one of the only sources
available for calculating spatial wind derivatives from satellites.
However, the methods used to calculate the derivatives have varied
between different studies and the assumptions used with different
calculation methods can have important implications for the features
that are resolved in the derivative fields. This talk gives a comparison
of the different methods to calculate wind derivatives from orbital
swath winds.
Oct. 3rd:
Kyra Britton: Application of High-Resolution Winter Seasonal Climate
Forecasts for Streamflow Prediction in Central Florida
Description: Current global climate models typically run at a resolution
of 100 km, which is too coarse to adequately resolve the coastlines and
watersheds of Florida. Previous researchers created a reforecast of five
environmental variables for a period of 22 years by dynamically
downscaling a global model, thus giving more accurate regional data for
temperature, evaporation, surface and root level soil moisture, and
surface temperature. In this project, I attempt to define the
relationship between these five reforecasted variables and the
streamflow of several watersheds in Central Florida using statistical
techniques, with the end goal of creating a streamflow forecast that
will assist water utility managers in decision making
Xiaobiao Xu:
Mark Bourassa: Current-Related Air-Sea Coupling
Nov. 7th
Joanna Rodgers: TBA
Tony Freveletti: TBA
TBA:TBA
Dec. 5th
Carly Narotsky: TBA
TBA: TBA
Shawn Smith: The MarineFlux project
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