F) Tropical cyclones forecasting

F1) What regions around the globe have tropical cyclones and who is responsible for forecasting there?
F2) What are those NWP "numerical weather products" or numerical models that the RSMC La Réunion talks about in the technical warnings and discussions ?
F3) What are the various forecasts that are being issued for seasonal tropical cyclone activity around the world ?
F4) How accurate are the forecasts from the RSMC La Réunion?

Subject F1) What regions around the globe have tropical cyclones and who is responsible for forecasting there?

Contributed by Chris Landsea and Anne-Claire Fontan

WMO

There are seven tropical cyclone "basins" where storms occur on a regular basis:

  1. Atlantic basin (including the North Atlantic Ocean, the Gulf of Mexico, and the Caribbean Sea)
  2. Northeast Pacific basin (from Mexico to about the dateline)
  3. Northwest Pacific basin (from the dateline to Asia including the South China Sea)
  4. North Indian basin (including the Bay of Bengal and the Arabian Sea)
  5. Southwest Indian basin (from Africa to about 100E)
  6. Southeast Indian/Australian basin (100E to 142E)
  7. Australian/Southwest Pacific basin (142E to about 120W)

The 6 WMO recognized Regional Specialized Meteorological Centers (RSMC) for Hurricanes/Typhoons and 6 Tropical Cyclone Warning Centers (TCWC) provide the official tropical cyclone guidance track and intensity forecasts for their designated areas. These are:

  1. RSMC Miami. The National Hurricane Center in Miami, Florida, USA has responsibilities for monitoring and forecasting tropical cyclones in the Atlantic and Northeast Pacific basin east of 140W.
  2. RSMC Honolulu. The Central Pacific Hurricane Center in Honolulu has responsibilities for the remainder of the Northeast Pacific basin from 140W to 180 degrees longitude.
  3. RSMC Tokyo. The Japanese Meteorological Agency Typhoon Center has the responsibility for the northwest Pacific Ocean basin.
  4. RSMC New Delhi. The Indian Meteorological Agency Cyclone Center in New Delhi has responsibilities for the North Indian Ocean basin.
  5. RSMC La Reunion. The French Meteorological office in La Reunion has responsibilities for the Southwest Indian Ocean basin.
  6. RSMC Nadi. The Fijian Meteorological Service office in Nadi, Fiji has the responsibility for the southwest Pacific Ocean.
  1. TCWC Perth (Australia) issues advisories for the area 10S-40S/90E-110E
  2. TCWC Darwin (Australia) for the area 125E-142E
  3. TCWC Brisbane (Australia) for the Coral Sea between 142E and 160E
  4. TCWC Wellington (New Zealand) for the southwest Pacific Ocean basin south of 25S
  5. TCWC Port-Moresby (Papua New Guinea) for the area 0S-10S/141E-160E
  6. TCWC Jakarta (Indonesia) for the area 0S-10S/90E-125E.
In the different basins, some National Meteorological Services (NMSs) provide tailored forecasts for their areas: Note also that the US Joint Typhoon Warning Center (JTWC) issues warnings for tropical cyclones in the Northwest Pacific, the North Indian, the Southwest Indian, the Southeast Indian/Australian, and the Australian/Southwest Pacific basins, though they are not specifically tasked to do so by the WMO. The US Naval Pacific Meteorology and Oceanography Center in Pearl Harbor, Hawaii does the same for the Pacific Ocean east of 180E (Neumann 1993).

Note that on rare occasions, tropical cyclones (or storms that appear to be similar in structure to tropical cyclones) can develop in the Mediterranean Sea. These have been noted to occur in September 1947, September 1969, January 1982, September 1983, and, most recently, during 13 to 17 January, 1995. Some study of these storms has been reported on by Mayengon (1984) and Ernest and Matson (1983), though it has not been demonstrated fully that these storms are the same as those found over tropical waters. It may be that these Mediterranean tropical cyclones are more similar in nature to polar lows.

The recent hurricane that formed in the South Atlantic was handled by the Brazilian weather service. Since tropical cyclones are so rare in this region, the WMO has not designated a forecast center with responsibility for there.

The following are the addresses of tropical cyclone centers listed above that are responsible for issuing advisories and/or warnings on tropical cyclones (thanks to Jack Beven for these):

World Meteorological Organization WWW: http://www.wmo.ch/web/www/TCP/rsmcs.html

OAR

Mail: 11691 SW 17th St. Miami, FL 33165-2149 USA
WWW: http://www.nhc.noaa.gov/index.html

Central Pacific Hurricane Center

Mail: National Weather Service Forecast Office Central Pacific Hurricane Center 2525 Correa Rd. Suite 250 Honolulu, HI 96822 USA WWW:http://www.prh.noaa.gov/cphc

Joint Typhoon Warning Center

Mail: NAVPACMETOCCEN/JTWC 425 Luapele Rd. Pearl Harbor, HI 96860 USA
WWW: http://www.npmoc.navy.mil/

Regional Specialized Meteorological Center Tokyo, Japan - Typhoon Center

Mail: Japanese Meteorological Agency 1-3-4 Ote-machi, Chiyoda-ku Tokyo Japan
WWW: http://www.goin.nasda.go.jp/GOIN/JMA/

Hong Kong Observatory

Mail: 134A Nathan Road Kowloon Hong Kong
WWW: http://www.info.gov.hk/hko/index.htm

Bangkok Tropical Cyclone Warning Center - Thailand

Mail: Director Meteorological Department 4353 Sukumvit Rd. Bangkok 10260 Thailand

Fiji Tropical Cyclone Warning Center

Mail: Director Fiji Meteorological Services Private Mail Bag Nadi Airport Fiji

New Zealand Meteorological Service

Mail: Director Met Service PO Box 722 Wellington New Zealand
WWW: http://www.metservice.co.nz/index.asp

Port Moresby Tropical Cyclone Warning Center

Mail: Director National Weather Service PO Box 1240 Boroko, NCD Paupa New Guinea

Brisbane Tropical Cyclone Warning Center

Mail: Regional Director Bureau of Meteorology GPO Box 413 Brisbane 4001 Australia
WWW: http://www.bom.gov.au/weather/qld

Darwin Tropical Cyclone Warning Center

Mail: Regional Director Bureau of Meteorology Northern Territory Regional Office PO Box 40050, CASUARINA, N.T. 0801 Australia
WWW: http://www.bom.gov.au/weather/nt

Perth Tropical Cyclone Warning Center

Mail: Regional Director Bureau of Meteorology GPO Box 1370 West Perth,WA 6872 Australia
WWW: http://www.bom.gov.au/weather/wa

Jakarta, Indonesia

Mail: Director Analysis and Processing Centre Jalan Arief Rakhman Hakim 3 Jakarta Indonesia

Regional Specialized Meteorological Centre La Reunion, France - Tropical Cyclones Center

Mail: Director of Meteorological Services PO Box 4 97490 Sainte Clotilde La Reunion FRANCE
WWW: http://www.meteo.fr (Le temps/ Outre-mer/ La Reunion)

Sub-Regional Tropical Cyclone Warning Center - Mauritius

Mail: Director of Meteorological Service Vacoas Mauritius

Sub-Regional Tropical Cyclone Warning Center - Madagascar

Mail: Director of Meteorological Service PO Box 1254 Antananarivo 101 Madagascar

Nairobi, Kenya

Mail: Director of Meteorological Services PO Box 30259 Nairobi Kenya

Maputo, Mozambique

Mail: Director of Meteorology PO Box 256 Maputo Mozambique

The following cities are also mentioned as tropical cyclone warning centers, though I don't have the addresses for them.
Philippines:  Manila


China:        Beijing 
              Dalian
              Shanghai
              Guangzhou

Korea:        Seoul

Vietnam:      Hanoi

India:        New Delhi
              Calcutta 
              Bombay

Bangladesh:   Dhaka

Burma:        Rangoon


Sri Lanka:    Colombo

Maldive Islands: Male

Please refer to the section "links" to directly connect to some of the centres.


Subject F2) What are those NWP "numerical weather products" or numerical models that the RSMC La Réunion talks about in the technical warnings and discussions ?

Source Samuel Westrelin.

  1. ARPEGE-IFS is a common development between Météo-France and ECMWF. ARPEGE (Action de Recherche Petite Echelle Grande Echelle) is the French name while IFS (Integrated Forecast System) is the name used by ECMWF. It is a global stretched model with no tropical cyclone's initialization. There are 4 runs a day: 00, 06, 12, 18 UTC. 00 UTC run is up to range 102h, 06 UTC up to 72h, 12 UTC up to 84h, and 18 UTC up to 60h. The assimilation runs with a 6-hour cycle, and the analysis method is a four dimensional variational analysis for upper air fields. The time step is 900 seconds. The resolution varies from 15 km over France to 55 km over Reunion Island and 90 km over New-Zealand.

  2. ALADIN-Réunion is a model adapted on Southwest Indian ocean at La Réunion by the Cyclone Research Team of Météo-France but developed by 16 euro-mediterranean countries This is a limited area model that covers the [0°-32S] [31.5E – 88.5E] area with a resolution of 10km - horizontal mesh size: 400 (lat) x 648 (lon) points. The initialization of tropical cyclones is a bogus of synthetic wind observations from the surface to 500 hPa deduced from the Holland analytical model, plus the mean sea level pressure at the center. There are 2 runs a day : 00 and 12 UTC, both of them up to 84 hours.

  3. The European Centre for Medium-Range Weather Forecasts's global model (ECMWF) runs twice a day, at 00 and 12 UTC, up to 240h (http://www.ecmwf.int).

  4. The United Kingdom Meterological Office's global model (UKMET) is utilized for forecasting the track of tropical cyclones around the world (Radford 1994).

  5. The GFDL model is a triply-nested movable mesh primitive equation model developed at the Geophysical Fluid Dynamics Laboratory. Position centre (latitude/longitude) and minimal sea level pressure of the tropical cyclones given by this model are received at the RSMC La Réunion since cyclone season 2004-2005.

  6. The United States Navy Operational Global Atmospheric Prediction Systems (NOGAPS) is also a global numerical model that shows skill in forecasting tropical cyclone track (Fiorino et al. 1993). Position centre (latitude/longitude) and minimal sea level pressure of the tropical cyclones given by this model are received at the RSMC La Réunion since cyclone season 2004-2005.

  7. CONW is not strictly speaking a model but a consensus, i.e. an average of up to 8 models (depending on the availability of the models), computed by the American navy. Position centre (latitude/longitude) and minimal sea level pressure of the tropical cyclones given by this consensus are received at the RSMC La Réunion since cyclone season 2004-2005.

Subject F3) What are the various forecasts that are being issued for seasonal tropical cyclone activity around the world ?

Contributed by Stan Goldenberg

There are a number of different seasonal forecasts currently being issued for various basins. Some of these are fairly new, while the oldest and most well known ( Prof. Bill Gray's forecast from CSU) has been issued for almost two decades.


Subject F4) How accurate are the forecasts from the RSMC La Réunion?

Contributed by Anne-Claire Fontan.

The RSMC La Réunion issues an official forecast, every six hours, of the center position, maximum ten-minutes surface (10 meters elevation) wind speed (intensity), radii of the 34 knot, 50 knot, and 64 knot, wind speeds in four quadrants (northeast, southeast, southwest, and northwest) surrounding the system, minimal sea level pressure, system movement etc...
The RSMC La Réunion has been issuing predictions for the forecast periods of 12, 24, and 48 hours since 1990. Forecasts for 36, 60 and 72 hours were first issued in 2004. All official forecast are verified by comparison with the "best track", a set of six-hour center positions, maximum wind speed values, minimal sea level pressure and T/Ci Dvorak numbers, that represents the official RSMC estimate of the location and intensity of a system. A best track is prepared for every system, after the fact, using all available data.

Fig. 1 Yearly-average official track forecast errors for 00-,12, 24 ,36, 48, 60, and72-hours, southwestern Indian ocean basin, including all intensities, since cyclone season 1990-1991.

RSMC La Réunion's official track errors have averaged in the last few years about 100 km at 12 hr, 150 km at 24 hr and 300 km at 48 hr. One can see that RSMC La Réunion has even done better than these numbers since 2005. Forecasts are now also issued at 3 lead time. These are average errors so, of course, individual predictions may be substantially better or worse. It is to the researchers community that these predictions have gotten so much better in the last few years, due to a combination of more accurate numerical models, and a better understanding of the physics of hurricane movement.

The improvements in intensity predictions are much slower than in the track predictions. Much work still remains to better understand and predict wind intensity changes in tropical storms and hurricanes.