synoptic chart - translation to ολλανδικά
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synoptic chart - translation to ολλανδικά

1000-KM-ORDER METHOD OF MEASURING WEATHER SYSTEMS
Synoptic Scale; Synoptic scale; Synoptic meteorology; Synoptic chart

synoptic chart         
een overzicht gevende kaart (kaart die het weer aangeeft op een bepaald moment (in meteorologie))
synoptic weather chart         
  • Sir [[Francis Galton]], the inventor of the weather map
  • US weather map from 1843
TABLE OF WEATHER ELEMENTS
Weather maps; Weather chart; Meteorological chart; Synoptic weather chart
verkorte weerkaart
weather map         
  • Sir [[Francis Galton]], the inventor of the weather map
  • US weather map from 1843
TABLE OF WEATHER ELEMENTS
Weather maps; Weather chart; Meteorological chart; Synoptic weather chart
weerkaart

Ορισμός

Weather map
·add. ·- A map or chart showing the principal meteorological elements at a given hour and over an extended region. Such maps usually show the height of the barometer, the temperature of the air, the relative humidity, the state of the weather, and the direction and velocity of the wind. Isobars and isotherms outline the general distribution of temperature and pressure, while shaded areas indicate the sections over which rain has just fallen. Other lines inclose areas where the temperature has fallen or risen markedly. In tabular form are shown changes of pressure and of temperature, maximum and minimum temperatures, and total rain for each weather station since the last issue, usually 12 hours.

Βικιπαίδεια

Synoptic scale meteorology

In meteorology, the synoptic scale (also known as large scale or cyclonic scale) is a horizontal length scale of the order of 1000 kilometers (about 620 miles) or more. This corresponds to a horizontal scale typical of mid-latitude depressions (e.g., extratropical cyclones). Most high- and low-pressure areas seen on weather maps (such as surface weather analyses) are synoptic-scale systems, driven by the location of Rossby waves in their respective hemisphere. Low-pressure areas and their related frontal zones occur on the leading edge of a trough within the Rossby wave pattern, while high-pressure areas form on the back edge of the trough. Most precipitation areas occur near frontal zones. The word synoptic is derived from the Greek word συνοπτικός (synoptikos), meaning seen together.

The Navier–Stokes equations applied to atmospheric motion can be simplified by scale analysis in the synoptic scale. It can be shown that the main terms in horizontal equations are Coriolis force and pressure gradient terms; therefore, one can use geostrophic approximation. In vertical coordinates, the momentum equation simplifies to the hydrostatic equilibrium equation.