CIRRUSWeb Login 

Home
Up
What's New
Climate Information
Services
Education
Special Projects
About Us
Search

 

SE Regional Climate Center
2221 Devine St., Suite 222
Columbia, SC 29205
Toll Free:
1-866-845-1553
Phone:
803-734-9560
          
803-734-9559
Fax:
803-734-9573
sercc@dnr.state.sc.us

 

 

Southern AER

A Quarterly Activity Bulletin of The South Carolina Department of Natural Resources-Southeast Regional Climate Center
Summer 2000
Volume 6, No. 2

How to Read A Weather Map

Information about Weather Maps

The information displayed on a weather map is used to illustrate processes that are continuously occurring in the atmosphere. The majority of these processes are not visible to the naked eye, so symbols are used to represent their location on a map. The symbols are designed to convey a large amount of weather information on a limited amount of map space. Weather maps illustrate current weather such as cloud coverage, precipitation, thunderstorms, high and low pressure systems, wind speed and wind direction. Fronts are also illustrated on weather maps. Fronts are boundaries between warm and cold air masses. A great deal of information can be gathered from a weather map by understanding the various symbols used to describe the weather conditions.

Spatial Patterns of Meteorological Variables

Meteorological variables, such as temperature, dew point, and barometric (atmospheric) pressure, have spatial distributions which can be displayed on a map. The use of isolines is commonly used for highlighting spatial patterns of specific variables. An isoline is a line of constant value: isotherms are lines of constant temperature; isodrosotherms are lines of constant dew point; and isobars are lines of constant barometric pressure. There are several generalizations that can be made about isolines:

h Because isolines represent constant values, they do not cross.

h Isolines should be relatively smooth.

h Isolines are commonly positioned at 4-mb intervals, centered on 1000-mb for barometric pressure and     intervals of 5E F for temperature and dew point.

Air Masses Influencing Weather in North America

An air mass is a large body of air with relatively uniform temperature and humidity. An air mass forms over large bodies of land or water and take on the characteristics of that surface. Air masses that form over land are referred to as continental while air masses forming over large water bodies are referred to as maritime, reflecting the high moisture continent found in them. Air masses are also classified by their temperature characteristics. Depending on where they form, an air mass may be described as equatorial, tropical, polar, or arctic. When two unlike air masses meet, the boundary between the them is called a front. A cold front is when cold air overtakes an area of warmer air, and a warm front is used to describe a warm air mass moving into an area of cooler air. Weather events such as cloud formation, precipitation, thunderstorms, and wind generally develop near a frontal boundary.

Pressure Systems and Wind

The air that makes up the atmosphere is not evenly distributed around the earth. An area that has a higher concentration of air is referred to as an area of high pressure, while an area with a lower concentration of air is referred to as an area of low pressure. On a weather map, pressure systems are labeled with an H for high pressure and an L for low pressure. Air moves from areas of high pressure to areas of low pressure creating wind. This is because the atmosphere constantly strives to obtain an equilibrium, or equal air pressure, around the earth. Air moves clockwise around a high pressure system and counter-clockwise around a low pressure system. Therefore wind speed and direction can be estimated by knowing the location of high and low pressure systems on a weather map. The weather map below illustrates high and low pressure systems as well as frontal boundaries.

Map Symbols

Symbols are used on weather maps to illustrate where weather phenomenon are occurring. These symbols represent wind speed and direction, the various types of precipitation, and the percent of cloud cover. A weather station is depicted on a map by a circle. Numbers around the station symbol indicate the temperature, dew point, and pressure.

The value for temperature is located on the upper left side of the station symbol, dew point on the lower left. The value for pressure is located to the upper right of the station symbol. The value represents the last three digits of the observed pressure. If the value is greater than 500, the initial 9 is missing, if the value is less than 500 the initial 10 is missing. The pressure is determined by placing the 9 or 10 in front of the reported value and dividing by 10.

For example:

A pressure value of 129 becomes 1012.9.

A pressure value of 759 becomes 975.9.

The amount of the circle filled in represents the amount of cloud cover at that location. Wind speed is shown on a weather map by various symbols. Calm conditions is depicted by two open circles, one inside the other. Winds 1-2 mph is depicted by a straight line and wind speeds above that are depicted by one or more barbs and/or triangles attached to a straight line. These symbols are referred to as wind barbs. The wind direction is indicated by the flat end of the wind barb, which will point into the station. The figure below depicts a weather station reporting five-tenths sky coverage and winds blowing from the northwest at 21-25 mph. This symbol also shows a temperature of 86 degrees, a dew point of 76, and a pressure of 1012.9.

The figures below show map symbols wind, sky coverage, and precipitation.


Activity Questions

1. An isotherm is a line of constant __________________.

2. What is an air mass that forms over land referred to as?

3. What is the boundary between two unlike air masses called?

4. Which way does air rotate around a high pressure system?

5. Look at the below graphic and determine the following weather variables:

Temperature

Dew Point

Pressure

Wind Speed

Wind Direction

Sky Cover

6. Pick the weather station closest to your town and determine the weather as depicted on map below. Use the same variables listed in number 5.

Permission is granted for the reproduction of materials contained in this bulletin.

Southern AER
Southeast Regional Climate Center
S.C. Department of Natural Resources
1201 Main Street, Suite 1100
Columbia, South Carolina 29201

The South Carolina Department of Natural Resources prohibits discrimination on the basis of race, color, sex, national origin, disability, religion, or age. Direct all inquiries to the Office of Human Resources, P.O. Box 167, Columbia, SC 29202.

 

 

sercc@dnr.state.sc.us