Glossary of tropical cyclone terms
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The following is a glossary of tropical cyclone terms.
A
- Advisory
- Official information issued by tropical cyclone warning centers describing all tropical cyclone watches and warnings in effect along with details concerning tropical cyclone locations, intensity and movement, and precautions that should be taken. Advisories are also issued to describe: (a) tropical cyclones prior to issuance of watches and warnings and (b) subtropical cyclones.
B
- Best track
- A subjectively-smoothed representation of a tropical cyclone's location and intensity over its lifetime. The best track contains the cyclone's latitude, longitude, maximum sustained surface winds, and minimum sea-level pressure at 6-hourly intervals. Best track positions and intensities, which are based on a post-storm assessment of all available data, may differ from values contained in storm advisories. They also generally will not reflect the erratic motion implied by connecting individual center fix positions.
C
- Center
- Generally speaking, the vertical axis of a tropical cyclone, usually defined by the location of minimum wind or minimum pressure. The cyclone center position can vary with altitude. In advisory products, refers to the center position at the surface.
- Center / Vortex Fix
- The location of the center of a tropical or subtropical cyclone obtained by reconnaissance aircraft penetration, satellite, radar, or synoptic data.
- Central North Pacific Basin
- The region north of the Equator between 140W and the International Dateline. The Central Pacific Hurricane Center (CPHC) in Honolulu, Hawaii is responsible for tracking tropical cyclones in this region.
- Coriolis force
- The fictitious force that causes the apparent deflection of an object that is moving in a straight line in an inertial reference frame as perceived by an observer in a rotating reference frame. The effect of this force is at its minimum at the equator and increases away from it. In the synoptic scales of the atmosphere, the Coriolis force will cause flow flowing towards a low pressure area to deflect perpendicularly to the pressure gradient driving the flow.[1] This causes the flow to rotate cyclonically about its center, producing geostrophic flow.[2] Tropical cyclones require a minimum distance of 500 km (310 mi) from the equator to sustain tropical cyclogenesis.[3]
- Cyclone
- An atmospheric closed circulation rotating counter-clockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere.
D
- Direct hit
- A close approach of a tropical cyclone to a particular location. For locations on the left-hand side of a tropical cyclone's track (looking in the direction of motion), a direct hit occurs when the cyclone passes to within a distance equal to the cyclone's radius of maximum wind. For locations on the right-hand side of the track, a direct hit occurs when the cyclone passes to within a distance equal to twice the radius of maximum wind. Compare indirect hit, strike.
E
- Eastern North Pacific Basin
- The portion of the North Pacific Ocean east of 140W. The National Hurricane Center in Miami, Florida is responsible for tracking tropical cyclones in this region.
- Eye
- The roughly circular area of comparatively light winds that encompasses the center of a severe tropical cyclone. The eye is either completely or partially surrounded by the eyewall cloud.
- Eyewall / Wall Cloud
- An organized band or ring of cumulonimbus clouds that surround the eye, or light-wind center of a tropical cyclone. Eyewall and wall cloud are used synonymously.
- Extratropical
- A term used in advisories and tropical summaries to indicate that a cyclone has lost its "tropical" characteristics. The term implies both poleward displacement of the cyclone and the conversion of the cyclone's primary energy source from the release of latent heat of condensation to baroclinic (the temperature contrast between warm and cold air masses) processes. It is important to note that cyclones can become extratropical and still retain winds of hurricane or tropical storm force.
- Extratropical cyclone
- A cyclone of any intensity for which the primary energy source is baroclinic, that is, results from the temperature contrast between warm and cold air masses.
F
- Fujiwhara effect
- The tendency of two nearby tropical cyclones to rotate cyclonically about each other.
G
- Gale Warning
- A warning of 1/10-minute sustained surface winds in the range 34 kn (39 mph or 63 km/h) to 47 kn (54 mph or 87 km/h) inclusive, either predicted or occurring and not directly associated with tropical cyclones.
H
- High Wind Warning
- A high wind warning is defined as 1-minute average surface winds of 35 kn (40 mph or 64 km/h) or greater lasting for 1 hour or longer, or winds gusting to 50 kn (58 mph or 93 km/h) or greater regardless of duration that are either expected or observed over land.
- HURDAT
- The short name for the Hurricane Database, the database for all tropical cyclones in the Atlantic Ocean, Gulf of Mexico, and Caribbean Sea since 1851, and the Northeast Pacific Ocean since 1949.[4]
- Hurricane / Typhoon
- A tropical cyclone in which the maximum sustained surface wind (using the U.S. 1-minute average) is 64 kn (74 mph or 119 km/h) or more. The term hurricane is used for Northern Hemisphere tropical cyclones east of the International Dateline to the Greenwich Meridian. The term typhoon is used for Pacific tropical cyclones north of the Equator west of the International Dateline.
- Hurricane Local Statement
- A public release prepared by local National Weather Service offices in or near a threatened area giving specific details for its county/parish warning area on (1) weather conditions, (2) evacuation decisions made by local officials, and (3) other precautions necessary to protect life and property.
- Hurricane Season
- The portion of the year having a relatively high incidence of hurricanes. The hurricane season in the Atlantic, Caribbean, and Gulf of Mexico runs from June 1 to November 30. The hurricane season in the Eastern Pacific basin runs from May 15 to November 30. The hurricane season in the Central Pacific basin runs from June 1 to November 30.
- Hurricane Warning
- An announcement that hurricane conditions (sustained winds of 74 mph or higher) are expected somewhere within the specified coastal area. Because hurricane preparedness activities become difficult once winds reach tropical storm force, the hurricane warning is issued 36 hours in advance of the anticipated onset of tropical-storm-force winds.
- Hurricane Watch
- An announcement that hurricane conditions (sustained winds of 74 mph or higher) are possible within the specified coastal area. Because hurricane preparedness activities become difficult once winds reach tropical storm force, the hurricane watch is issued 48 hours in advance of the anticipated onset of tropical-storm-force winds.
I
- Indirect Hit
- Generally refers to locations that do not experience a direct hit from a tropical cyclone, but do experience hurricane force winds (either sustained or gusts) or tides of at least 4 feet above normal.
- Inland Tropical Storm Warning
- The equivalent of a Tropical Storm Warning for inland counties, put into use after multiple Tornado Warnings were issued for Hurricane Katrina, when tornadoes were not present, but winds were the equivalent of EF0-2 tornadoes. These are issued by local NWS forecast offices, not the NHC.
- Inland Hurricane Warning
- The equivalent of a Hurricane Warning for inland counties, put into use after multiple Tornado Warnings were issued for Hurricane Katrina, when tornadoes were not present, but winds were the equivalent of EF0-2 tornadoes. These are issued by local NWS forecast offices, not the NHC.
- Invest
- A weather system for which a tropical cyclone forecast center (NHC, CPHC, or JTWC) is interested in collecting specialized data sets (e.g., microwave imagery) and/or running model guidance. Once a system has been designated as an invest, data collection and processing is initiated on a number of government and academic web sites, including the Naval Research Laboratory (NRL) and the University of Wisconsin Cooperative Institute for Meteorological Satellite Studies (UW-CIMSS). The designation of a system as an invest does not correspond to any particular likelihood of development of the system into a tropical cyclone; operational products such as Tropical Weather Outlooks or Significant Tropical Weather Advisories should be consulted for this purpose.
K
- Kelvin wave
- An eastward moving atmospheric wave that can enhance deep convection and contribute to tropical cyclogenesis, especially over the Pacific Ocean. They towards the east at about 10° to 20° longitude per day.
L
- Landfall
- The intersection of the surface center of a tropical cyclone with a coastline. Because the strongest winds in a tropical cyclone are not located precisely at the center, it is possible for a cyclone's strongest winds to be experienced over land even if landfall does not occur. Similarly, it is possible for a tropical cyclone to make landfall and have its strongest winds remain over the water. Compare direct hit, indirect hit, and strike.
M
- Major hurricane
- A designation used by the National Hurricane Center reserved for hurricanes in the Atlantic or Northeast Pacific basins that achieve Category 3 in the Saffir–Simpson Hurricane Scale. These storms have winds of at least 96 knots (178 km/h; 111 mph).[5]
O
- Outflow
- Air that flows outwards from a storm system; associated with ridging, or anticyclonic flow. Low-level outflow boundaries from mesoscale convective complexes can disrupt the center of small tropical cyclones.[6] However, outflow aloft is essential for the strengthening of a tropical cyclone.[7] If this outflow is undercut, the tropical cyclone weakens. If two tropical cyclones are in proximity, the upper level outflow from the system to the west can limit the development of the system to the east.[8]
P
- Philippine Area of Responsibility
- An area bounded by rhumb lines on the Philippine Tropical Cyclone Tracking Chart/Map or imaginary lines on the surface of the earth that makes equal oblique angles with all meridians joining the following points: 25°N 135°E, 25°N 120°E, 5°N 135°E, 5°N 115°E, 15°N 115°E, and 21°N 120°E. Tropical cyclone bulletins are issued by the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) every six or twelve hours for all tropical cyclones within this area.
- Post-storm Report
- A report issued by a US National Weather Service office summarizing the impact of a tropical cyclone on its forecast area. These reports include information on observed winds, pressures, storm surges, rainfall, tornadoes, damage and casualties.
- Post-tropical Cyclone
- A former tropical cyclone. This generic term describes a cyclone that no longer possesses sufficient tropical characteristics to be considered a tropical cyclone. Post-tropical cyclones can continue carrying heavy rains and high winds. Note that former tropical cyclones that have become fully extratropical...as well as remnant lows...are two classes of post-tropical cyclones.
- Preliminary Report
- Now known as the "Tropical Cyclone Report". A report summarizing the life history and effects of an Atlantic or eastern Pacific tropical cyclone. It contains a summary of the cyclone life cycle and pertinent meteorological data, including the post-analysis best track (six-hourly positions and intensities) and other meteorological statistics. It also contains a description of damage and casualties the system produced, as well as information on forecasts and warnings associated with the cyclone. NHC writes a report on every tropical cyclone in its area of responsibility.
- Present Movement
- The best estimate of the movement of the center of a tropical cyclone at a given time and given position. This estimate does not reflect the short-period, small scale oscillations of the cyclone center.
R
- Radius of maximum wind
- The distance from the center of a tropical cyclone to the location of the cyclone's maximum winds. In well-developed hurricanes, the radius of maximum winds is generally found at the inner edge of the eyewall.
One of the quantities used to determine the size of a tropical cyclone. The ROCI is determined by measuring the radii from the center of the storm to its outermost closed isobar in four quadrants, which is then averaged to come up with a scalar value. It generally delimits the outermost extent of a tropical cyclone's wind circulation.[9]
- Rapid deepening
- An increase in the maximum sustained winds of a tropical cyclone of at least 30 kn in a 24-h period.
- Relocated
- A term used in an advisory to indicate that a vector drawn from the preceding advisory position to the latest known position is not necessarily a reasonable representation of the cyclone's movement.
- Reformed
- A term used in an advisory to indicate that the center of a tropical cyclone, usually weak, has dissipated and a new center has formed at a different location. This will sometimes lead to an incorrect representation of movement. The center of a cyclone can reform multiple times in its life. The new center is not given a new name, unless there is a period of time between old center dissipation and new center reformation.
- Remnant Low
- A post-tropical cyclone that no longer possesses the convective organization required of a tropical cyclone...and has maximum sustained winds of less than 34 knots. The term is most commonly applied to the nearly deep-convection-free swirls of stratocumulus in the eastern North Pacific.
S
| Category | Wind Speed | Damage |
|---|---|---|
| 1 | 74 - 95 | Very dangerous winds will produce some damage |
| 2 | 96 - 110 | Extremely dangerous winds will cause extensive damage |
| 3 | 111 - 130 | Devastating damage will occur |
| 4 | 131 - 155 | Catastrophic damage will occur |
| 5 | > 155 | Catastrophic damage will occur |
- Saffir-Simpson Hurricane Scale/Saffir-Simpson Hurricane Wind Scale
- The Saffir-Simpson Hurricane Wind Scale is a 1 to 5 categorization based on the hurricane's intensity at the indicated time. The scale provides examples of the type of damage and impacts in the United States associated with winds of the indicated intensity. The following table shows the scale broken down by winds:
- Sea surface temperature
- Water temperature close to the surface of a large body of water, such as an ocean or sea. Normally, an ocean temperature of 26.5 °C (79.7 °F) spanning through at least a 50-metre depth is one of the six requirements needed to maintain the special mesocyclone that is the tropical cyclone.[3] These warm waters are needed to maintain the warm core that fuels tropical systems.
- Severe Tropical Storm
- A term used by the Japan Meteorological Agency to describe a typhoon with 10-minute windspeeds between 88–117 km/h (55–73 mph).
- Severe Typhoon
- A term used by the Hong Kong Observatory to describe a typhoon with 10-minute windspeeds between
- Storm surge
- An abnormal rise in sea level accompanying a hurricane or other intense storm, and whose height is the difference between the observed level of the sea surface and the level that would have occurred in the absence of the cyclone. Storm surge is usually estimated by subtracting the normal or astronomic high tide from the observed storm tide.
- Storm tide
- The actual level of sea water resulting from the astronomic tide combined with the storm surge.
- Storm Warning
- A warning of 1-minute sustained surface winds of 48 kn (55 mph or 88 km/h) or greater, either predicted or occurring, not directly associated with tropical cyclones.
- Strike
- strike zone diagram For any particular location, a hurricane strike occurs if that location passes within the hurricane's strike circle, a circle of 125 nmi diameter, centered 12.5 nmi to the right of the hurricane center (looking in the direction of motion). This circle is meant to depict the typical extent of hurricane force winds, which are approximately 75 nmi to the right of the center and 50 nmi to the left.
- Subtropical cyclone
- A non-frontal low pressure system that has characteristics of both tropical and extratropical cyclones. This system is typically an upper-level cold low with circulation extending to the surface layer and maximum sustained winds generally occurring at a radius of about 100 miles or more from the center. In comparison to tropical cyclones, such systems have a relatively broad zone of maximum winds that is located farther from the center, and typically have a less symmetric wind field and distribution of convection.
- Subtropical Depression
- (Atlantic/Eastern Pacific Ocean) - A subtropical cyclone in which the maximum sustained surface wind speed is 33 kn (38 mph or 62 km/h) or less.
- Subtropical Depression
- (South-West Indian Ocean) - a named or unnamed subtropical cyclone.
- Subtropical Storm
- A subtropical cyclone in which the maximum sustained surface wind speed (using the U.S. 1-minute average) is 34 kn (39 mph or 63 km/h) or more.
- Super Tropical Cyclone
- A term used by RSMC Nadi and the Tropical Cyclone Warning Centers in Perth, Darwin, Jakarta, Port Moresby and Wellington, to describe an Australian category 3, 4 or 5 tropical cyclone that has windspeeds greater than 120 km/h (75 mph).
- Super Typhoon (CMA)
- A term used by the China Meteorological Administration, to describe a typhoon in the Western Pacific that has sustained windspeeds greater than over a 3-minute period
- Super Typhoon (HKO)
- A term used by the Hong Kong Observatory, to describe a typhoon in the Western Pacific that has sustained windspeeds greater than over a 10-minute period
- Super Typhoon (JTWC)
- A term used by the Joint Typhoon Warning Center in the Western Pacific, to describe a typhoon that has sustained windspeeds greater than 130 knots over a 1-minute period.
- Super Typhoon (PAGASA)
- A term used by PAGASA to unofficially describe a typhoon in the Western Pacific, that the Joint Typhoon Warning Center has called a Super Typhoon.
- Synoptic flights
- Weather reconnaissance mission flown to provide vital meteorological information in data sparse ocean areas as a supplement to existing surface, radar, and satellite data. Synoptic flights better define the upper atmosphere and aid in the prediction of tropical cyclone development and movement.
T
- Tropical cyclogenesis
- Tropical cyclogenesis is the technical term that describes the development and strengthening of a tropical cyclone in the atmosphere.[10] Tropical cyclogenesis involves the development of a warm-core cyclone, due to significant convection in a favorable atmospheric environment.[11] There are six main requirements for tropical cyclogenesis: sufficiently warm sea surface temperatures, atmospheric instability, high humidity in the lower to middle levels of the troposphere, enough Coriolis force to develop a low pressure center, a preexisting low level focus or disturbance, and low vertical wind shear.[3]
- Tropical cyclone
- A warm-core non-frontal synoptic-scale cyclone, originating over tropical or subtropical waters, with organized deep convection and a closed surface wind circulation about a well-defined center. Once formed, a tropical cyclone is maintained by the extraction of heat energy from the ocean at high temperature and heat export at the low temperatures of the upper troposphere. In this they differ from extratropical cyclones, which derive their energy from horizontal temperature contrasts in the atmosphere (baroclinic effects).
- Tropical depression
- A tropical cyclone in which the maximum sustained surface wind speed (using the U.S. 1-minute average) is 33 kn (38 mph or 62 km/h) or less.
- Tropical disturbance
- A discrete tropical weather system of ostensibly organized convection—generally 100 to 300 nmi in diameter—originating in the tropics or subtropics, having a non-frontal migratory character, and maintaining its identity for 24 hours or more. It may or may not be associated with a detectable perturbation of the wind field.
- Tropical storm
- A tropical cyclone in which the maximum sustained surface wind speed (using the U.S. 1-minute average) ranges from 34 kn (39 mph or 63 km/h) to 63 kn (73 mph or 118 km/h).
- Tropical Storm Warning
- An announcement that tropical storm conditions (sustained winds of 39 to 73 mph) are expected somewhere within the specified coastal area within 36 hours.
- Tropical Storm Watch
- An announcement that tropical storm conditions (sustained winds of 39 to 73 mph) are possible within the specified coastal area within 48 hours.
- Tropical wave
- A trough or cyclonic curvature maximum in the trade-wind easterlies. The wave may reach maximum amplitude in the lower middle troposphere.
- Typhoon
- A tropical cyclone with winds exceeding 74 mph (118 km/h) in the western Pacific Ocean, the equivalent of a hurricane
W
- Western North Pacific Basin
- The portion of the North Pacific Ocean from 100E to 180E. The Joint Typhoon Warning Center in Pearl Harbor, Hawaii, and the Japan Meteorlogical Agency are both responsible for tracking tropical cyclones in this region
References
- ↑ Department of Atmospheric Sciences (1999-10-04). "Pressure Gradient Force". University of Illinois at Urbana-Champaign. Retrieved 2006-10-20.
- ↑ Roger Graham Barry & Richard J. Chorley (2003). Atmosphere, Weather and Climate. Routledge. p. 115. ISBN 0-415-27171-1.
- 1 2 3 Chris Landsea. "How do tropical cyclones form?". Frequently Asked Questions: Hurricanes, Typhoons and Tropical Cyclones. Atlantic Oceanographic and Meteorological Laboratory. Retrieved 2006-07-25.
- ↑ National Hurricane Center (May 2011). "NHC Archive of Hurricane Seasons". National Oceanic and Atmospheric Administration. Retrieved 2011-07-04.
- ↑ National Hurricane Center (2006-06-02). "Saffir-Simpson Hurricane Scale Information". National Oceanic and Atmospheric Administration. Retrieved 2007-02-25.
- ↑ John A. Knaff and John F. Weaver (September 2000). "A Mesoscale Low-Level Thunderstorm Outflow Boundary Associated with Hurricane Luis". Monthly Weather Review. American Meteorological Society. 128: 3352–3355. Bibcode:2000MWRv..128.3352K. doi:10.1175/1520-0493(2000)128<3352:AMLLTO>2.0.CO;2.
- ↑ National Weather Service (September 2006). "Hurricanes... Unleashing Nature's Fury: A Preparedness Guide" (PDF). National Oceanic and Atmospheric Administration. Archived from the original (PDF) on 2008-02-26. Retrieved 2010-04-09.
- ↑ Dr. Harold P. Gerrish (1989). "Preliminary Report: Tropical Storm Iris - 16–21 September 1989". National Hurricane Center. Retrieved 2010-04-08.
- ↑ FRÉDÉRIC MOUTON and OLA NORDBECK. Cyclone Database Manager. Retrieved on 2008-07-14.
- ↑ Arctic Climatology and Meteorology. "Definition for Cyclogenesis". National Snow and Ice Data Center. Retrieved 2006-10-20.
- ↑ Goldenberg, Stan (August 13, 2004). "What is an extra-tropical cyclone?". Frequently Asked Questions: Hurricanes, Typhoons and Tropical Cyclones. Atlantic Oceanographic and Meteorological Laboratory. Retrieved 2008-08-30.
This article incorporates public domain material from the NOAA document "Glossary of NHC Terms".
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