Introduction to 500 mb maps

Introduction

In this class we will mainly be viewing what are called 500 mb height maps (recall that mb stands for millibars, which is a unit for measuring air pressure). These maps are very good for getting a large-scale picture of the "weather pattern" over the United States, North America, or even the Northern Hemisphere. 500 mb maps are most applicable for studying winter time weather patterns in the middle latiutudes (between about 30° and 60° latitude). This is why I waited until mid October to cover this topic. The purpose of this page is to begin to show you how to interpret the height patterns (contour lines) that are plotted on the maps.

Where to get Maps

If you do a web search for weather maps, you will find hundreds (maybe thousands) of sites containing maps. If you are interested, you should check some out. You should go through this exercise of looking at maps. I will expect you to be able to answer simple questions about how to do this on the exam. If you become interested in looking at these maps, you can continue to visit the site listed below outside of this class.

I suggest using the University of Wyoming's weather model plotting page. I will give you some directions on how to use the plotting software to make 500 mb maps. Open another browser window and type in the following address, then follow the instructions:
http://weather.uwyo.edu/models/fcst

Select one of the six forecast models listed to go to the map page
Set the Initial time to the latest time and date available
Weather observations from around the whole world are used in forecast models, so everything must be coordinated to a standard time. The standard is to use Greenwich Mean Time (also called Zulu time) in military format (00-24 hours each day). The Zulu time (labeled with a Z) is always used on these weather maps. The Tucson local time is 7 hours earlier than Zulu time.
Some examples:
At 12Z, it is 0500 hours in Tucson (5AM).
At 00Z, it is 1700 hours in Tucson (5PM) the day before. This is a little tricky, but 00Z is midnight Zulu time and 7 hours before midnight is 5PM the day before.
Set the Region to either the United States or North America
Set the Forecast to 0 hours to see the conditions at the initial time, 24 hours to see the model forecast one day into the future, 48 hours to see the model forecast two days into the future, etc. If you select "loop", you will see a movie of the forecast.
Set the Level to 500 mb.
Until you are more familiar with the maps, you should make the following selections to see the 500 mb height pattern:
First color fill --> None Second color fill --> None First contour --> Heights Second contour --> None Vector --> None
Once all selections are made, click GET DATA to produce the map

After you are familiar with how to use the map page, follow the link below to directly connect:
University of Wyoming's weather model page

Estimating temperature from 500 mb pattern

The height contours on the map are actually the height of the 500 mb pressure surface above sea level. The average air pressure near the ground is about 1013 mb, and since air pressure decreases as one moves upward, at some altitude the air pressure will fall to 500 mb. Notice that the height contours generally fall into the range 4600 - 6000 meters.

For now, I want you to be able to estimate the pattern of air temperatures based on the pattern of height contours shown on the map. The height of the 500 mb surface is directly related to the temperature of the atmosphere below 500 mb -- the higher the temperature, the higher the height of the 500 mb level. We already discussed this when we were going over hurricanes. If you warm a column of air, it expands, therefore air pressure decreases more slowly as you ascend through a warm column of air, compared to a cold column of air. We will review this during lecture (See Figure).

In other words, the 500 mb height at any point on the map tells us about the average air temperature in the vertical column of air between the ground surface and the 500 mb height plotted at that point. The height pattern tells us where the air is relatively cold and where it is relatively warm.

Consider what the 500 mb pattern would look like if air temperatures decreased steadily from the equator toward the north pole. (Note this is what you might guess based on the fact that the Sun's heating is strongest toward the south and weakest toward the north.) In that case the height contours would be concentric circles around the north pole with the highest heights to the south (toward the equator). While this is generally true, the actual pattern at any given time is wavy. Where the height lines bow northward (a ridge), warm air has moved north; and where the height lines bow southward (a trough), cold air has moved south. Therefore, in general warmer than average temperatures can be expected underneath ridges and colder than average temperatures can be expected underneath troughs (See Figure). The more pronounced the ridge (or trough), the more above (or below) average the temperatures will be.

The terminology "trough" and "ridge" is related to the fact that the contour lines often look like waves. A "ridge" is the high point of a wave, and a "trough" is the low point of a wave. A simple diagram is shown below. Additional maps and diagrams will be used in lecture to help you understand what is meant by this.

To be a little more precise in estimating expected temperature compared to average, we should compare the actual 500 mb heights from a map to the long-term average or "climatological" 500 mb heights. For a given location, if the 500 mb height on the map is close to average, then the temperature is expected to be about average. If the 500 mb height is lower than the average height, then lower than average temperatures are expected. If the 500 mb height is higher than the average height, then higher than average temperatures are expected. The further the 500 mb height is away from average the more the temperature is expected to be away from average. For example, if you compare the actual 500 mb height over Tucson for a given day (say October 11) to the average 500 mb height (from the link below), you can estimate whether or not the air temperature for the day will be above or below average.

Below are some links to the averge long-term or climatological 500 mb heights for North America for the months October, November, and December.
October 500 mb height climatology (long-term average)
November 500 mb height climatology (long-term average)
December 500 mb height climatology (long-term average)

Notice (from looking at the links above) that the average 500 mb heights get lower as the winter season approaches. For example, over Tucson, the average heights fall from about 5800 m in October to about 5750 m in November to about 5700 m in December.

To give you an idea about how the 500 mb heights are related to temperature, we will look at the 500mb map for October 19, 1952. On that day the record high temperature for Tucson (for October 19) was recorded. It reached 99°F. The 500mb height over Tucson on October 19, 1952 was about 5900 m. This is well above the average of 5800 m for the month of October. The unusually high 500 mb height, corresponds with a very warm day.
500 mb map for October 19, 1952

Note of Caution:

This is a simplistic method. The 500 mb height actually tells you about the average air temperature in the vertical column of air between the ground surface and 4.6 - 6.0 km (2.9 - 3.8 miles) above sea level. Often this provides a good estimate of how warm or cold the air temperature is near the ground where we live. However, the vertical column of air from ground to 3 miles above sea level does not have to be uniformly warm or cold. There can be smaller (in vertical extent) layers of relatively warm air and relatively cold air. Sometimes there will be shallow (small in vertical dimension) layers of warm or cold air just above the ground. In these cases, the corresondence between the 500 mb height and surface air temperature will not work as well. In addition, factors like cloud cover, precipitation, and the type of ground surface (dry desert, moist soil, snow cover, etc.) also influence the temperature of the air at the surface. Thus, using the 500 mb heights to estimate surface temperatures is not exact. However, as you will see, the 500 mb maps often provide a very good overview of the pattern of warm and cold conditions near the ground surface.

Examples:

Below are two examples that were used in previous classes. The first is the 500 mb height map for the time 00Z on Monday, October 25, 2004 (This corresponds to a local Tucson time of 5 PM on Sunday, October 24). Next to the 500 mb map is the high temperature relative to average for the day Sunday, October 24. Notice that below average temperatures occured in the western US (associated with the trough over this region), while above average temperatures occured over the midwest southward to the southern great plains and lower Mississippi valley (associated with the ridge over this region), and below average temperatures over parts of the east coast (associated with the trough centered just offshore).

The next example is from January 14, 2007. The 500 mb map is valid for Sunday, January 14, 2007 at 18Z (this corresponds to 11 AM local Tucson time). Next to the 500 mb map is a map showing the surface temperatures across the United States at 20:15 GMT (or 20:15 Z, which is 13:15 (i.e., 1:15 PM) local time). Again, notice that temperatures are cool or cold near the trough in the western United States, for example 42°F in Tucson at 1:15 PM local time. In most of the southeastern United States, temperautures are much warmer in association with a broad ridge and higher 500 mb heights.

Additional examples will be provided in lecture.