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MESOSCALE LOW [7 records]

Record 1 2022-08-31

English

Subject field(s)
  • Atmospheric, Climatic and Meteorological Phenomena
DEF

A midlevel, warm-core low pressure center that develops within the stratiform region of a mesoscale convective system(MCS) as a result of latent heat release over a multihour time period.

Key term(s)
  • meso-scale convective vortex

French

Domaine(s)
  • Phénomènes météorologiques, climatiques et atmosphériques

Spanish

Save record 1

Record 2 2012-12-13

English

Subject field(s)
  • Atmospheric Physics
CONT

A second type of subtropical cyclone is a mesoscale low originating in or near a frontolyzing zone of horizontal wind shear, with [a] radius of maximum sustained winds generally less than 30 miles.

French

Domaine(s)
  • Physique de l'atmosphère

Spanish

Save record 2

Record 3 2012-12-12

English

Subject field(s)
  • Atmospheric Physics
CONT

A second type of subtropical cyclone is a mesoscale low originating in or near a frontolyzing zone of horizontal wind shear, with radius of maximum sustained winds generally less than 30 miles. The entire circulation may initially have a diameter of less than 100 miles. These generally short-lived systems may be either cold core or warm core.

French

Domaine(s)
  • Physique de l'atmosphère
CONT

«Warm-core» (cœur chaud) signifie que le cœur de la dépression est relativement plus chaud que son environnement pour une même surface de pression (une «surface de pression» étant une autre manière de mesurer la hauteur ou l'altitude).

Spanish

Save record 3

Record 4 2012-12-10

English

Subject field(s)
  • Atmospheric Physics
CONT

A second type of subtropical cyclone is a mesoscale low originating in or near a frontolyzing zone of horizontal wind shear, with radius of maximum sustained winds generally less than 30 miles. The entire circulation may initially have a diameter of less than 100 miles. These generally short-lived systems may be either cold core or warm core.

French

Domaine(s)
  • Physique de l'atmosphère
OBS

Structurellement, dans les cyclones tropicaux, les vents les plus forts se situent près du sol (conséquence d'être un «warm-core» dans la troposphère), alors que dans les dépressions des latitudes moyennes, les vents les plus forts sont près de la tropopause (conséquence d'être un «warm-core» dans la stratosphère et un «cold-core» dans la troposphère).

Spanish

Save record 4

Record 5 2012-11-27

English

Subject field(s)
  • Atmospheric Physics
CONT

A second type of subtropical cyclone is a mesoscale low originating in or near a frontolyzing zone of horizontal wind shear, with radius of maximum sustained winds generally less than 30 miles. The entire circulation may initially have a diameter of less than 100 miles. These generally short-lived systems may be either cold core or warm core.

French

Domaine(s)
  • Physique de l'atmosphère

Spanish

Save record 5

Record 6 2012-11-21

English

Subject field(s)
  • Atmospheric Physics
CONT

A second type of subtropical cyclone is a mesoscale low originating in or near a frontolyzing zone of horizontal wind shear, with radius of maximum sustained winds generally less than 30 miles.

Key term(s)
  • meso-scale low

French

Domaine(s)
  • Physique de l'atmosphère
Key term(s)
  • dépression de mésoéchelle

Spanish

Save record 6

Record 7 1992-12-31

English

Subject field(s)
  • Atmospheric, Climatic and Meteorological Phenomena
DEF

Small, shallow depression which forms mainly in winter over some high-latitude seas within a polar or arctic air mass.

CONT

When arctic-origin air in winter flows southward (northward in the southern hemisphere) across (relatively) warmer seas, strong surface heating acts both to enhance the degree of instability, and trigger vigorous moist convective towers. This is sufficient alone to give rise to heavy, wintry showers/cumulonimbus clusters etc., but often marked troughing, or even a closed circulation in the isobaric flow is found; the resultant low-level convergence/positive vorticity enhancement, plus the localised concentration of the latent heat energy released, enhances development within the system, and an intense (but synoptically small) area of rain, hail, sleet or snow & squally winds can result - a polar low (or polar depression or polar meso-cyclone in some texts).

CONT

What is a polar low? Part of a diverse group of mesoscale weather systems(polar meso-cyclones).... [There is] three types of polar meso-cyclones :-jet streak type,-arctic front type,-cold low type.

OBS

Polar mesocyclones: a term now used to encompass the whole ’family’ of disturbances resulting from arctic air flowing equatorward over progressively warmer seas; the term ’polar low’ is now often used only for ’extreme’ systems where gale or near gale-force winds are observed.

OBS

Its motion is approximately the same as the air stream in which it is embedded.

Key term(s)
  • polar meso cyclone

French

Domaine(s)
  • Phénomènes météorologiques, climatiques et atmosphériques
DEF

Petite dépression peu profonde qui se forme principalement en hiver dans une masse d'air polaire ou arctique située sur certaines mers des hautes latitudes.

OBS

Son mouvement est approximativement le même que celui du courant atmosphérique dans lequel elle se situe.

Spanish

Campo(s) temático(s)
  • Fenómenos meteorológicos, climáticos y atmosféricos
DEF

Depresión pequeña y poco profunda que se forma dentro de una masa de aire polar o ártico, especialmente en invierno, sobre los mares polares.

OBS

Se mueve siguiendo, aproximadamente, la dirección de la corriente de aire en que está inserta.

Save record 7

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