How to Read a Weather Map

 

Weather maps provide a simplified depiction of the current or predicted weather of an area. The most common weather map you will come across is surface analysis, which is what will be discussed here. Reading a surface analysis weather map can seem difficult at first, but with a little practice you’ll be able to do it in no time.

 

Understand general concepts of the weather. What most people are concerned with is precipitation, which, in meteorology (the study of weather), is any form of water that falls onto the Earth's surface. Forms of precipitation include rain, hail, snow, and sleet. High pressure implies fair weather and low pressure is usually associated with precipitation.

 

Study a weather map. Watch out for one on the TV news, online, or in your local newspaper. (Other sources may include magazines and books, but they may not be current.) Newspapers are a convenient method to find a weather map as they are cheap, reliable, and can be cut apart so you can carry them with you while learning to interpret the symbols.[1]

 

Analyze a small portion of your weather map. If possible, find a map covering a smaller area – these can be easier to interpret. Focusing on a larger scale may be difficult for a beginner. On the map, notice the location, lines, arrows, patterns, colors, and numbers. Every sign counts and all are different.

 

Reading the Air Pressure

Understand what air pressure measures. This is the weight or pressure the air exerts on the ground and is measured in millibars. It is important to be able to read air pressure because pressure systems are associated with certain weather patterns.

 

Learn the air pressure symbols. To read air pressure on a surface analysis weather map, check for isobars (iso = equal, bar = pressure) – plain, curved lines that indicate areas of equal air pressure. Isobars play a major role in determining the speed and direction of wind.[2]

  • When the isobars form concentric closed (but not always round) circles, the smallest circle in the center indicates a pressure center. This can be either a high-pressure system (depicted by an "H" in English, "A" in Spanish) or a low pressure system (depicted by an "L" in English, "B" in Spanish).[3]
  • Air does not flow "down" pressure gradients; it flows "around" them due to the Coriolis effect (Earth spinning). Hence, wind direction is indicated by the isobars, counterclockwise around lows (cyclonic flow) and clockwise around highs (anticyclonic) in the northern hemisphere, thus creating wind. The closer the isobars are to one another, the stronger the winds.

 

Learn how to interpret a Low Pressure System (Cyclone). These storms are characterized by increased cloudiness, winds, temperatures, and chance of precipitation. They are represented on a weather map by isobars that are close together with arrows traveling clockwise (Southern Hemisphere) or counter-clockwise (Northern Hemisphere), usually with a "T" in the middle isobar, which forms a round circle (the letter can vary, however, depending on the language the weather report is presented in).[4]

  • Radar imagery can show low-pressure systems. Tropical cyclones (South Pacific) are also named hurricanes around America or typhoons in coastal Asia.

 

Learn how to interpret a High Pressure System. These conditions indicate clear, calm weather with reduced chance of precipitation. Drier air usually results in a greater range of high and low temperatures.[5]

  • They are represented on a weather map as isobars with an "H" in the middle isobar and arrows showing which direction the wind is flowing (clockwise in Northern Hemisphere, counter-clockwise in the Southern Hemisphere). Like cyclones, they can also be shown with radar imagery.

 

Interpreting the Types of Fronts

 

Observe the types and movement of fronts. These mark the boundary between warmer air on one side and colder air on the other. If you are close to a front and you know the front is moving towards you, you can expect a change in weather (e.g. cloud formation, precipitation, thunderstorms, and wind) when the front boundary passes over you. Mountains and large bodies of water can distort its path. On a weather map, you will notice some lines that have semi-circles or triangles on either side, or both (shown here). These indicate the boundaries for various types of fronts.[6]

 

Analyze a Cold front. With these weather patterns, rainfall can be torrential and wind speeds can be high. Blue lines with triangles on one side represents cold fronts on weather maps. The direction the triangles point is the direction in which the cold front is moving.[7]

 

Analyze a Warm front. These often bring a gradual increase in rainfall as the front approaches, followed by prompt clearing and warming after the front passes. If the warm air mass is unstable, the weather might be characterized by prolonged thunderstorms. A red line with semi-circles on one side represents warm fronts. The side the semi-circles are on represent the direction in which the warm front is heading.[8]

 

Study an Occluded front. These are formed when a cold front overtakes a warm front. They are associated with various weather events (possibly thunderstorms) depending on whether it is a warm or cold occlusion. The passing of an occluded front usually brings drier air (lowered dew point). A purple line with semi-circles and triangles both on the same side represents occluded fronts. Whichever side they're on, is the direction the occluded front is going.[9]

 

Analyze a Stationary front. These indicate a non-moving boundary between two different air masses. These fronts have long continuous rainy periods that linger for extended periods in one area and move in waves. A semi-circle bordering one side and triangles along the opposite side represents that the front is not moving in any direction.[10]

 

 

Interpreting Other Weather Map Symbols

 

Read the station models at each point of observation. If your weather map has station models, each one will plot the temperature, dew-point, wind, sea level pressure, pressure tendency, and ongoing weather with a series of symbols.[11]

  • Temperature is generally recorded in Celsius degrees and rainfall is recorded in millimeters. In the US, temperatures are in Fahrenheit and rainfall is measured in inches.
  • Cloud cover is indicated by the circle in the middle; the extent to which it is filled indicates the degree to which the sky is overcast.

Study the lines on the weather map. There are many other lines on weather maps. Two of the most important kinds of lines indicate isotherms and isotachs.[12]

  • Isotherms – These are lines on a weather map that connect points through which the isotherm passes have the same temperature.
  • Isotachs – These are lines on a weather map that connect points where the isotach passes have the same wind speed.

Analyze the pressure gradient. A number on the isobars, such as "1008", is thepressure (in millibars) along that line. The distance between isobars is referred to as the pressure gradient. A large change in pressure over a short distance (i.e. close isobars) indicates strong winds.[13]

 

Analyze wind strength. Wind barbs point in the direction of the wind. Lines or triangles coming off the main line at an angle indicate wind strength: 50 knots for every triangle, 10 knots for every full line, 5 knots for every half line.[14]

 

 

Sources and Citations

  1.  http://www.intellicast.com/National/Surface/Current.aspx
  2.  http://weather.n3ujj.com/How_to_Read_Weather_Maps.html
  3. http://www.crsol.com/weather_routing_toolkit/idtoolkit/resources/content/analyze_synoptic_weather_how.pdf
  4.  http://www.opc.ncep.noaa.gov/product_description/keyterm.shtml
  5.  http://www.metoffice.gov.uk/public/weather/surface-pressure/#?tab=surfacePressureColour&fcTime=1461798000
  6.  http://www.meteor.wisc.edu/~hopkins/aos100/sfc-anl.htm
  7.  http://www.wpc.ncep.noaa.gov/html/fntcodes2.shtml
  8.  http://www.srh.weather.gov/srh/jetstream/synoptic/wxmaps.html
  9.  http://www.wpc.ncep.noaa.gov/html/fntcodes2.shtml
  10.  http://www.srh.weather.gov/srh/jetstream/synoptic/wxmaps.html
  11.  http://profhorn.meteor.wisc.edu/wxwise/weather/lesson3/content_Station.html
  12.  https://climate.ncsu.edu/edu/k12/.IsobarIsotherm
  13.  http://www.theweatherprediction.com/habyhints2/475/
  14.  http://www.wpc.ncep.noaa.gov/html/stationplot.shtml

 

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