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For information on using this template, see Template:Routemap. For pictograms used, see Commons:BSicon/Catalogue . Note: Per consensus and convention, most route-map templates are used in a single article in order to separate their complex and fragile syntax from normal article wikitext.
This map shows the tracks of all tropical cyclones which formed worldwide from 1985 to 2005. The map was created with the WPTC track map generator by Nilfanion.. The track map generator program generates a track map from the NHC HURDAT data, [A 1] or from Automated Tropical Cyclone Forecast (ATCF) B-deck data files (commonly referred to as "best track" files).
Tropical storm [12] 1962 Tropical storm September 25, 1962: Tillie [10] Tropical storm [12] 1964 Remnant low September 9, 1964: Emily [11] Category 1 [12] 1965 Remnant low September 6, 1965: Kirsten [13] Tropical storm [12] 1966 Remnant low September 29, 1966: Katrina [6] Category 1 [12] 1967 Tropical storm August 29, 1967: Hyacinth [11 ...
The NHC official forecast for Ernesto (2006) is light blue, while the storm's actual track is the white line over Florida Main article: Automated Tropical Cyclone Forecasting System Historically, tropical cyclone tracking charts were used to include the past track and prepare future forecasts at Regional Specialized Meteorological Centers and ...
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Significant track errors still occur on occasion, as seen in this Ernesto (2006) early forecast. The NHC official forecast is light blue, while the storm's actual track is the white line over Florida. A tropical cyclone forecast model is a computer program that uses meteorological data to forecast aspects of the future state of tropical cyclones.
A 2008 government plan, updated in 2018, proposes four lines running at 30-minute headways during peak hours and 2-hour headways during off-peak hours. The commuter rail system would be complementary to the Phoenix–Tucson passenger rail project planned by the Arizona Department of Transportation and Amtrak. [1] [2]
Another example of a storm track is the circumpolar storm track in the Antarctic, however land-sea contrasts play no role in its formation. Given a grid point field of geopotential height , storm tracks can be visualized by contouring its average standard deviation , after the data has been band-pass filtered.