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The SLOSH basins have considerable overlap to allow for complete storm surge coverage for planning and operations. Jul 1, Version 6. This section briefly describes the scientific techniques used to create the seamless inundation maps for Category hurricanes using the SLOSH MOM product as well as a description of the datasets and map viewer available to the public. Virtual Program- Creativity in Motion.

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Recreation Commission. Summer Camp. Recreation Reimagined. Arrow Left Arrow Right. Looking for a unique place to take a walk? A paved sidewalk and a rubberized trail completely outlines the perimeter of Daffin Park and is 1. This is the southernmost boundary of the Historical District. Skip to content. Programming Schedule. Tracking the Vaccine. First Alert Weather. Astronomical Tide And River Data. Summer Weather Tips. End Zone. Outdoor Overhaul. SLOSH has been used operationally for more than three decades.

For planning purposes, the NHC uses a representative sample of hypothetical storms to estimate the near worst—case scenario of flooding for each hurricane category. MEOWs are created by computing the maximum storm surge resulting from up to , hypothetical storms simulated through each SLOSH grid of varying forward speed, radius of maximum wind, intensity Categories , landfall location, tide level, and storm direction. A MEOW product is created for each combination of category, forward speed, storm direction, and tide level.

For each storm combination, parallel storms make landfall in 5 to 10 mile increments along the coast within the SLOSH grid, and the maximum storm surge footprint from each simulation is composited, retaining the maximum height of storm surge in a given basin grid cell.

SLOSH MOMs are available for mean tide and high tide scenarios and represent the near worst-case scenario of flooding under ideal storm conditions. A high tide initial water level was used for the storm surge hazard maps.

SLOSH employs curvilinear polar, elliptical, and hyperbolic telescoping mesh grids to simulate the storm surge hazard. The spatial coverage for each SLOSH grid ranges from an area the size of a few counties to a few states. The resolution of individual grid cells within each basin ranges from tens to hundreds of meters to a kilometer or more.

Sub—grid scale water features and topographic obstructions such as channels, rivers, and cuts and levees, barriers, and roads, respectively are parameterized to improve the modeled water levels. Figure 1. SLOSH grids are not drawn to scale. In locations that have a steep and narrow continental shelf, wave setup can be a substantial contributor to the total water level rise observed during a tropical cyclone. Wave setup is defined as the increase in mean water level due to momentum transfer to the water column by waves that are breaking or otherwise dissipating their energy.

An accurate digital elevation model DEM takes considerable time, resources, and expertise to develop and is required to compute inundation. The following data may be collected but it is not linked to your identity:. Privacy practices may vary, for example, based on the features you use or your age. Learn More. With Family Sharing set up, up to six family members can use this app. App Store Preview. Screenshots iPad iPhone.

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If you discover via these maps that you live in an area vulnerable to storm surge, find out today if you live in a hurricane storm surge evacuation zone as prescribed by your local emergency management agency. If you do live in such an evacuation zone, decide today where you will go and how you will get there, if and when you're instructed by your emergency manager to evacuate. If you don't live in one of those evacuation zones, then perhaps you can identify someone you care about who does live in an evacuation zone, and you could plan in advance to be their inland evacuation destination — if you live in a structure that is safe from the wind and outside of flood-prone areas.

Storm surge information is provided to federal, state, and local partners to assist in a range of planning processes, risk assessment studies, and operational decision-making. In regards to the former, tens of thousands of climatology-based hypothetical tropical cyclones are simulated in each SLOSH basin or grid , and the potential storm surges are calculated. This section briefly describes the scientific techniques used to create the seamless inundation maps for Category hurricanes using the SLOSH MOM product as well as a description of the datasets and map viewer available to the public.

SLOSH has been used operationally for more than three decades. For planning purposes, the NHC uses a representative sample of hypothetical storms to estimate the near worst—case scenario of flooding for each hurricane category. MEOWs are created by computing the maximum storm surge resulting from up to , hypothetical storms simulated through each SLOSH grid of varying forward speed, radius of maximum wind, intensity Categories , landfall location, tide level, and storm direction. A MEOW product is created for each combination of category, forward speed, storm direction, and tide level.

For each storm combination, parallel storms make landfall in 5 to 10 mile increments along the coast within the SLOSH grid, and the maximum storm surge footprint from each simulation is composited, retaining the maximum height of storm surge in a given basin grid cell. SLOSH MOMs are available for mean tide and high tide scenarios and represent the near worst-case scenario of flooding under ideal storm conditions.

A high tide initial water level was used for the storm surge hazard maps. SLOSH employs curvilinear polar, elliptical, and hyperbolic telescoping mesh grids to simulate the storm surge hazard. The spatial coverage for each SLOSH grid ranges from an area the size of a few counties to a few states.

The resolution of individual grid cells within each basin ranges from tens to hundreds of meters to a kilometer or more.

Sub—grid scale water features and topographic obstructions such as channels, rivers, and cuts and levees, barriers, and roads, respectively are parameterized to improve the modeled water levels. Figure 1. SLOSH grids are not drawn to scale. In locations that have a steep and narrow continental shelf, wave setup can be a substantial contributor to the total water level rise observed during a tropical cyclone.

Wave setup is defined as the increase in mean water level due to momentum transfer to the water column by waves that are breaking or otherwise dissipating their energy.

An accurate digital elevation model DEM takes considerable time, resources, and expertise to develop and is required to compute inundation. Two datasets were used to create the DEM:. This minor level of smoothing provides a less noisy map that is easier to interpret, and ultimately a seamless DEM for storm surge inundation mapping. The native grid cell size for that data is about 3m and for the purposes of this analysis, that data was resampled to a grid cell size of about 9 meters.

In areas outside of the U. First, the usable areas of the SLOSH grids were reduced to ignore spurious data along the grid boundaries. The SLOSH basins have considerable overlap to allow for complete storm surge coverage for planning and operations. Merging these basins into a seamless product requires specialized technical considerations. Since the grid boundaries yield unreliable data, basin overlap was minimized, and the high-resolution and center portions of grids were retained.

Second, the maximum water levels in each MOM were merged onto a uniform grid for processing. High-quality maps are essential for effective risk communication. Using social science research, the carefully derived and high resolution inundation maps provide a means for effective risk communication and analysis. Bowles Ford is located just off Stiles Avenue, near the Cloverdale neighborhood.

Children are welcome; dogs on a leash are permitted. The site includes locks 5 and 6 of the original canal that began operation in Fernwood Dr. Floodways to Greenways is a new way of addressing drainage issues, combining Storm water infrastructure with community amenities like passive parks and gardens. The distance around the lake is. Highway 80 East, the trail provides 6 miles for hiking and biking between Bull River and Fort Pulaski. Download the Savannah Bicycle Campaign bicycle map. Heads Up Concussion.

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