Renseignements généraux

Nº de série

S/O

Nº de partie

1

Nombre total de parties

1

Ou

S/O

Brevets

S/O

Description générale

Synthetic

Dimensions

Remarque : Cette information reflète la taille générale pour l’entreposage et ne représente pas nécessairement les véritables dimensions de l’objet.

Longueur

16,4 cm

Largeur

10,7 cm

Hauteur

S/O

Épaisseur

S/O

Poids

S/O

Diamètre

S/O

Volume

S/O

Lexique

Groupe

Météorologie

Catégorie

Mesure de vitesse et direction du vent de surface

Sous-catégorie

S/O

Fabricant

Ou

Environment CA

Pays

Canada

État/province

Inconnu

Ville

Inconnu

Contexte

Pays

Canada

État/province

Inconnu

Période

Inconnu

Canada

An example of tool used by Canadian Meteorological Service. A piece of meteorological equipment from a large collection of meteorological instruments used by the Meteorological Service of Canada (previously Atmospheric Environment Service) and acquired by the CSTM since 1967. MSC is the government agency responsible for collecting and disseminating meteorological data and forecasts in Canada. It was founded in 1871 in Toronto where it is still headquartered. The MSC was originally on the University of Toronto downtown campus but moved to Downsview in 1971 on land owned by UofT. The headquarters houses laboratories, research facilities and calibration and instrument maintenance facilities (now largely contracted out).

Fonction

A protractor-like instrument used to compute geostrophic wind level using isobaric contours shown of surface weather maps in order to determine winds for aircraft operations or to determine maximum surface wind or gust.

Technique

This plastic geostrophic wind scale is used with a surface weather map. [The donor provided four of these maps to the museum in the same accession lot as this wind scale.] On these maps [there are . . .] isobars which are lines of equal pressure based on the sa level pressure. The station pressures are converted to sea level pressure (MSL) and plotted to the right and just above the station location. The forecaster uses these pressures to draw the isobars. Other factors are used to produce the exact placement of the lines. These isobars are drawn every 4 millibars, i.e. 996, 1000, 1004 etc. Those pressures would be plotted beside the station as 960, 000, and 040, i.e. the MSL pressure to the nearest 1/10 of a millibar. The nomial sea level pressure is 1010 millibars. Thus the pressure difference between any two isobards is four millibars. The winds above the planetary boundary layer, i.e. 3000 feet, follow the isobars. The direction is parallel to the isobars. According to Buy-Ballots Law, if the lowest pressure is on your left then the wind is at your back. The wind flow is counter clockwise around a low in the northern hemisphere. Based on these principles the protractor [found on the wind scale] is used to determine the 3000' wind direction. The distance between the isobars is inversely proportional to the wind speed at 3000' feet. But it also varies with latitude (coriolis force) which is why latitude and speed in knots are combined on the scale. The forecaster merely lays the transparent scale on the map and moves it as necessary to determine these winds [ Ken Devine, email correspondence].

Notes sur la région

Inconnu

Détails

Marques

Black lettering reads 'SEA LEVEL/ GEOSTROPHIC WIND/ SCALE' and 'ATMOSPHERIC ENVIRONMENT SERVICE/ DEPT. OF THE ENVIRONMENT - CANADA/ STOCK NO. 0026-2830'/ black markings for two scales

Manque

Complete

Fini

Colourless and transparent, yellowed

Décoration

S/O