Gulf of
Ruoying He1, Yizhen Li1, Dennis McGillicuddy2, Don Anderson2, Bruce Keafer2
1North
2Woods Hole Oceanographic Institution
Disclaimer: these simulations are for experimental purposes only.
Results here represent model solutions initiated from a cyst abundance map from October 2008, with germination, growth, and transport of Alexandrium fundyense cells driven by the factors listed below.
Physical
circulation model
Multiple nested ROMS, ca. ~1km resolution in GOM
Tides (M2, S2, N2,
6-hourly wind and heat fluxes from NOAA/NCEP NOMADS (35-km resolution)
River runoff data from USGS
Sea surface temperature from satellites
Initial conditions and open boundary conditions from large-scale parent model (HYCOM)
Alexandrium
fundyense model
Population dynamics from Stock et al. (2005); McGillicuddy et al. (2005), and He et al., (2008)
Cyst maps from Fall 2008 Survey in comparison with earlier years
(http://omglnx3.meas.ncsu.edu/yli/cystmap/cystmap_04_08.png)
Solar radiation from NOAA/NCEP
Monthly climatological nutrient fields from University of Maine
The mortality rate of A.
fundyense is now parameterized using the temperature dependent Q10
formulation (Durbin and Durbin, 1992)
An animation showing surface wind fields and modeled bloom conditions from February 1, 2009 to July 15, 12:00, 2009
http://omgsrv1.meas.ncsu.edu/GoMaine_Redtide/2009/weekly_nowcast_forecast/dino_09.htm
An 3-D animation showing modeled surface and subsurface cell abundance
from February 1, 2009 to July 5, 12:00, 2009
http://omgsrv1.meas.ncsu.edu/GoMaine_Redtide/2009/weekly_nowcast_forecast/09forecast_3d/dino_09.htm
Last update: July 13, 2009