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Hurricane Web Links
Here's a great link for up-to-the-minute Hurricane related data:
http://www.crownweather.com/tropical.html
Tropical Tracking Systems
Ever wonder what all the computer tracking models are and more importantly what they mean? Below is a brief introduction and a little background info on Tropical/Hurricane Tracking Models.
XTRAP -- simple extrapolated track. Assumes the storm just keeps going at the same speed and direction. No physics at all involved. Generally of no use except as a "what if" scenario.
BAMD -- deep layer Beta Advection Model. Good for strong storms in the lower tropics (south of 20N latitude where steering currents remain constant). It doesn't emply much, if any, physics to predict changes in steering currents. Because of that, it shoudl not be used where fronts/trofs highs/lows move on by (north of 20N latitude. Never use it in the Gulf or western Atlantic. NHC -- The official NHC forecast.
BAMM -- mid layer Beta Advection Model. For weaker to moderate-strength storms in the deep tropics. Same shortcomings as the BAMD model above. Don't use it north fo 20N. NHCA98E -- Climatology-based "model". Not really a model, just compares the current storm position to previous storms and "guesses" where it might go. Completely useless everywhere.
CLIPER -- CLImatology and PERsistence. No physics, not a real model. It's used by forecasters to determine if their forecasts have any skill at all. If you can't beat climatology and persistence, then you're not a very good forecaster.
LBAR -- Limited BARotropic. Limited alright, limited in its ability to forecast tropical cyclones. Generally ignore it. UKMET -- Generally not a bad model. It's put out by the United Kingdom met office. It's worth a look at, but tropical cyclones aren't its forte'. It is run twice daily at 12Z (7am CDT) and 00Z (7pm CDT)
GFDL -- Geophysical Fluid Dynamics Laboratory model. This model was designed for hurricanes. It's based upon the latest AVN (American GFS) model. Because of that, though, it may tend to erode ridges too quickly north of stronger cyclones, leading to a right of track bias toward early recurvature. The GFDL did very well with Katrina, better than most other models, in fact. I take a hard look at the GFDL when making a forecast, but it has been all over the place with its forecast for Rita.
NOGAPS -- US Navy NOGAPS model. Designed for marine use, mostly. Sometimes does OK with tropical cyclones. Certainly worth a look. Run only twice daily so it's not available as often as other models.
CMC -- Canadian Model. I've never been too fond of this model. It may be good for winter up in Canada, but it's never shown me any expertise with tropical systems. If it gets a storm right, it's just usually pure luck: http://weatheroffice.ec.gc.ca/model_forecast/global_e.html
NAM/ETA -- The new North American Model (the ETA was renamed recently). One of the worst models out there for the tropics, and just about everything else. Recent "improvements" have really made this model pretty bad for use down south. Ignore it laugh at it, but don't use it to predict the path of a tropical cyclone.
So, of all the models above, the GFDL is one of the better models. But, like I said, it's was all over the place with the Rita track so far and I don't trust it much yet.
I also like to look at the American GFS model for comparison: http://www.nco.ncep.noaa.gov/pmb/nwprod/analysis/index_carib.shtml The GFS model certainly has its shortcomings, but if one knows its strengths/weaknesses, it can be a very good tool. Don't just trust it as-is unless you know what you're doing.
The European model (ECMWF) is a good tool. Here's a link to a site I like to use for the 7-day ECMWF: http://weather.cod.edu/forecast/loop.ecmwf850t.html
MM5 -- Florida State's MM5 model is definitely worth a look. It's a "home brew" model tweaked by FSU mets. Doesn't have too much of a track record, though: http://moe.met.fsu.edu/mm5/ Sometimes, the best models are what we call "ensemble" or "consensus" models. Simple "consensus" models just take 2-3 different models and simply average the positions for each time step out to 3-5 days to come up with a "consensus track".
Occasionally, this consensus is better than any one model. Some examples of consensus models: GUNA - GFDL, UKMET, NOGAPS, AVN (GFS) GUNS - GFDL, UKMET, NOGAPS More complex "ensemble" models actually analyze a number of models, account for each model's individual weaknesses, combine/average the tracks, then produce a single forecast track. You've probably heard of the Florida Superensemble model. This model has done VERY well with many tropical cyclones. Unfortunately, it's not available to the general public.
Here's a link to a good model page. It has a variety of models, from BAMs to various iterations of the GFDL model, to the GFS model, and some consensus model. Just weed out the "trash" models when looking at it: http://euler.atmos.colostate.edu/~vigh/guidance/
DEFINITIONS
Accumulated Cyclone Energy
– (ACE) A measure of a named storm’s potential for wind and storm surge destruction defined as the sum of the square of a named storm’s maximum wind speed (in 104 knots2) for each 6-hour period of its existence. The 1950-2000 average value of this parameter is 96.Atlantic Basin
– The area including the entire North Atlantic Ocean, the Caribbean Sea, and the Gulf of Mexico.El Niño
– (EN) A 12-18 month period during which anomalously warm sea surface temperatures occur in the eastern half of the equatorial Pacific. Moderate or strong El Niño events occur irregularly, about once every 3-7 years on average.Hurricane
– (H) A tropical cyclone with sustained low-level winds of 74 miles per hour (33 ms-1 or 64 knots) or greater.Hurricane Day
– (HD) A measure of hurricane activity, one unit of which occurs as four 6-hour periods during which a tropical cyclone is observed or estimated to have hurricane intensity winds.Intense Hurricane
- (IH) A hurricane which reaches a sustained low-level wind of at least 111 mph (96 knots or 50 ms-1) at some point in its lifetime. This constitutes a category 3 or higher on the Saffir/Simpson scale (also termed a "major" hurricane).Intense Hurricane Day
– (IHD) Four 6-hour periods during which a hurricane has an intensity of Saffir/Simpson category 3 or higher.Named Storm
– (NS) A hurricane or a tropical storm.Named Storm Day
– (NSD) As in HD but for four 6-hour periods during which a tropical cyclone is observed (or is estimated) to have attained tropical storm intensity winds.NTC
– Net Tropical Cyclone Activity –Average seasonal percentage mean of NS, NSD, H, HD, IH, IHD. Gives overall indication of Atlantic basin seasonal hurricane activity. The 1950-2000 average value of this parameter is 100.QBO
– Quasi-Biennial Oscillation – A stratospheric (16 to 35 km altitude) oscillation of equatorial east-west winds which vary with a period of about 26 to 30 months or roughly 2 years; typically blowing for 12-16 months from the east, then reversing and blowing 12-16 months from the west, then back to easterly again.Saffir/Simpson (S-S) Category
– A measurement scale ranging from 1 to 5 of hurricane wind and ocean surge intensity. One is a weak hurricane; whereas, five is the most intense hurricane.SOI
– Southern Oscillation Index – A normalized measure of the surface pressure difference between Tahiti and Darwin.SST(s)
– Sea Surface Temperature(s)SSTA(s)
– Sea Surface Temperature(s) AnomaliesTropical Cyclone
– (TC) A large-scale circular flow occurring within the tropics and subtropics which has its strongest winds at low levels; including hurricanes, tropical storms and other weaker rotating vortices.Tropical Storm
– (TS) A tropical cyclone with maximum sustained winds between 39 (18 ms-1 or 34 knots) and 73 (32 ms-1 or 63 knots) miles per hour.ZWA
– Zonal Wind Anomaly – A measure of the upper level (~200 mb) west to east wind strength. Positive anomaly values mean winds are stronger from the west or weaker from the east than normal.1 knot = 1.15 miles per hour = 0.515 meters per second