Since the Met office is no long “doing” or interested in the weather I grabbed what little there is about weather fronts from the Internet just s that the unlucky can have some point of reference to the North Atlantic charts.
Fortunately the USA is still golden:
Terminology and Weather Symbols
The leading edge of a relatively colder air mass which separates two air masses in which the gradients of temperature and moisture are maximized. In the northern hemisphere winds ahead of the front will be southwest and shift into the north-west with frontal passage.
The formation of a front occurs when two adjacent air masses with different densities and temperatures meet and strengthen the discontinuity between the air masses. It occurs most frequently over continental land areas such as over the Eastern US when the air mass moves out over the ocean. It is the opposite of frontolysis.
Frontolysis -The weakening or dissipation of a front occurs when two adjacent air masses lose contrasting properties such as the density and temperature. It is the opposite of frontogenesis.
Occluded frontThe union of two fronts, formed as a cold front overtakes a warm front or quasi-stationary front refers to a cold front occlusion. When a warm front overtakes a cold front or quasi-stationary front the process is termed a warm front occlusion. These processes lead to the dissipation of the front in which there is no gradient in temperature and moisture.
Ridgean elongated area of relatively high pressure that is typically associated with a anti-cyclonic wind shift.
Stationary frontA front that has not moved appreciably from its previous analyzed position.
Trough[Trof], an elongated area of relatively low pressure that is typically associated with a cyclonic wind shift.
The leading edge of a relatively warmer surface air mass which separates two distinctly different air masses. The gradients of temperature and moisture are maximized in the frontal zone. Ahead of a typical warm front in the northern hemisphere, winds are from the southeast and behind the front winds will shift to the southwest.
LOW & HIGH PRESSURE SYSTEMS AND MISCELLANEOUS KEY TERMS USED
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Low pressure with a number such as 99 means 999 mb and with 03 means 1003 mb. High pressure with a number such as 25 means 1025 mb.
Extratropical lowA low pressure center which refers to a migratory frontal cyclone of center and higher latitudes. Tropical cyclones occasionally evolve into extratropical lows losing tropical characteristics and become associated with frontal discontinuity.
Low pressureAn area of low pressure identified with counterclockwise circulation in the northern hemisphere and clockwise in the southern hemisphere. Also, defined as a cyclone.
High pressureAn area of higher pressure identified with a clockwise circulation in the northern hemisphere and a counterclockwise circulation in the southern hemisphere. Also, defined as an anticyclone.
NewThe term “NEW” may be used in lieu of a forecast track position of a high or low pressure center when the center is expected to form by a specific time. For example, a surface analysis may depict a 24-hour position of a new low pressure center with an “X” at the 24-hour position followed by the term “NEW”, the date and time in UTC which indicates the low is expected to form by 24 hours.
Rapidly intensifyingIndicates an expected rapid intensification of a cyclone with surface pressure expected to fall by at least 24 millibar (mb) within 24 hours.
Click for information on coding used with the surface preliminary analysis or for a list of “present weather” symbols.
SquallA sudden wind increase characterized by a duration of minutes and followed by a sudden decrease in winds.
Windspeed & Direction
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Fog -Over the marine environment the term fog refers to visibility greater than or equal to 1/2 NM and less than 3 NM. Fog is the visible aggregate of minute water droplets suspended in the atmosphere near the surface.
Dense fog -Over the marine environment the term dense fog refers to visibility less than 1/2 NM. Fog is the visible aggregate of minute water droplets suspended in the atmosphere near the surface. Usually dense fog occurs when air that is lying over a warmer surface such as the Gulf Stream is advected across a colder water surface and the lower layer of the air mass is cooled below its dew point.
Sea fogCommon advection fog caused by transport of moist air over a cold body of water.
FREEZING SPRAY and ICE EDGE
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Freezing spraySpray in which supercooled water droplets freeze upon contact with exposed objects below the freezing point of water. It usually develops in areas with winds of at least 25 knots.
Categories of Freezing Spray/Icing Light Moderate Heavy
Less than 0.7 cm/hr 0.7 cm/hr to less than or equal to 2.0 cm/hr Greater than 2.0 cm/hr
Less than 0.3 ins/hr 0.3 ins/hr to less than or equal to 0.8 ins/hr Greater than 0.8 ins/hr
Ice EdgeRepresented by a blue dotted line and is defined by the National Ice Center. It depicts the extent of ice coverage 10% or greater.
Freezing Spray and Ice Accretion example image
CONVENTIONS USED WITH WARNINGS FOR EXTRATROPICAL SYSTEMS
An area in which gale/storm force winds are forecast or are occurring, but in which more than one center is the generating these winds. Developing Gale -Refers to an extratropical low or an area in which gale force winds of 34 knots (39 mph) to 47 knots (54 mph) are “expected” by a certain time period. On surface analysis charts, a “DEVELOPING GALE” label indicates gale force winds within the next 24 hours. When the label is used on the 48 hour surface forecast and 96 hour surface forecast charts, gale force winds are expected to develop by 72 hours and 120 hours, respectively.
Developing Storm -Refers to an extratropical low or an area in which storm force winds of 48 knots (55 mph) to 63 knots (73 mph) are “expected” by a certain time period. On surface analysis charts, a “DEVELOPING STORM” label indicates storm force winds forecast within the next 24 hours. When the label is used on the 48 hour surface and 96 hour surface charts, storm force winds are expected to develop by 72 hours and 120 hours, respectively.
Developing Hurricane Force -Refers to an extratropical low or an area in which hurricane force winds of 64 knots (74 mph) or higher are “expected” by a certain time period. On surface analysis charts, a “DEVELOPING HURRICANE FORCE” label indicates hurricane force winds forecast within the next 24 hours. When the label is used on the 48 hour surface and 96 hour surface charts, hurricane force winds are expected to develop by 72 hours and 120 hours, respectively.
GaleRefers to an extratropical low or an area of sustained surface winds (averaged over a ten minute period, momentary gusts may be higher) of 34 knots (39 mph) to 47 knots (54 mph).
StormRefers to a extratropical low or an area of sustained winds (averaged over a ten minute period, momentary gusts may be higher) of 48 knots (55 mph) to 63 knots (73 mph).
Hurricane ForceRefers to a extratropical low or an area of sustained winds (averaged over a ten minute period, momentary gusts may be higher) in excess of 64 knots or higher(74 mph).
Small Craft Advisory
Refers to areas within the coastal waters with sustained winds of 18 knots (21 mph) to 33 knots (38 mph).
Heavy Freezing Spray
Spray in which supercooled water droplets freeze upon contact with exposed objects below the freezing point of water at the rate of greater than 2 cm/hr. It usually develops in areas with winds of at least 25knots.
CONVENTIONS USED WITH WARNINGS FOR TROPICAL SYSTEMS
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HurricaneA tropical cyclone with closed contours, a strong and very pronounced circulation, and one minute maximum sustained surface winds 64 knots (74 mph) or greater. A system is called a hurricane over the North Atlantic, Gulf of Mexico, North Pacific E of the dateline, and the South Pacific E of 160E.
Intertropical Convergence Zone(ITCZ) The region where the northeasterly and southeasterly trade winds converge, forming an often continuous band of clouds or thunderstorms near the equator.
Post-TropicalA cyclone that no longer possesses sufficient tropical characteristics to be considered a tropical cyclone. Post-tropical cyclones can continue carrying intense rainfalls and high winds. [Note that former tropical cyclones that have become fully extra-tropical, as well as remnant lows, are two classes of post-tropical cyclones. The term “post-tropical” is predominantly a convenient communications term–to permit the ongoing use of the storm name.]
Tropical cycloneA non-frontal, warm-core, low pressure system of synoptic scale, developing over tropical or subtropical waters with definite organized convection (thunderstorms) and a well defined surface wind circulation.
Tropical depressionA tropical cyclone with one or more closed isobars and a one minute max sustained surface wind of less than 34 knots (39 mph).
Tropical stormA tropical cyclone with closed isobars and a one minute max sustained surface wind of 34 knots (39 mph) to 63 knots (73 mph).
TyphoonSame as a hurricane with exception of geographical area. A tropical cyclone with closed contours, a strong and very pronounced circulation, and one minute maximum sustained surface winds of 64 knots (74 mph) or greater. A system is defined as a typhoon over the North Pacific W of the dateline.
NOTE: It can be difficult to determine the central pressures of tropical depressions, tropical storms, and hurricanes/typhoons and at times no estimates or measurements is provided by a hurricane or typhoon specialist. An estimate of central pressure may be provided over the Atlantic. Otherwise an XXX is used in place of actual or estimated pressures associated with these systems and an XX is used for forecast central pressure.
Combined seas -The combination of both wind waves and swell which is generally referred to as “seas”.
Primary swell directionPrevailing direction of swell propagation. Significant wave heightThe average height (trough to crest) of the 1/3rd highest waves. An experienced observer will most frequently report the highest 1/3rd of the waves observed. The generation of waves on water results not in a single wave height but in a spectrum of waves distributed from the smallest capillary waves to larger waves. Within this spectrum there is a finite possibility of each of the wave heights to occur with the largest waves being the least likely. The wave height most commonly observed and forecast is the significant wave height. This is defined as the average of the one third highest waves. The random nature of waves implies that individual waves can be substantially higher than the significant wave height. In fact, observations and theory show that the highest individual waves in a typical storm with typical duration to be approximately two times the significant wave height. Some reported rogue waves are well within this factor of two envelope. Waves higher than roughly twice the significant wave height fall into the category of extreme or rogue waves. SwellWind waves that have moved out of their fetch or wind generation area. Waves generated by swell exhibit a regular and longer period than wind waves.
Coastal WatersIncludes the area from a line approximating the mean high water along the mainland or island as far out as sixty nautical miles including the bays, harbors and sounds.High SeasThat portion of the Atlantic and Pacific oceans which extends off the Western and Eastern US coasts and extends to 35W in the Atlantic ocean and to 160E in the Pacific Ocean. The area includes both the coastal and offshore waters.Offshore watersThat portion of oceans, gulfs, and seas beyond coastal waters extending to a specified distance from the coastline, to a specified depth contour, or covering an area defined by a specific latitude and longitude points.
I feel like smacking the usual bastards in the face
So I will try to repair this another day.