A front is the boundary between two different airmasses. Air masses are categorized by their temperature and moisture properties. Let's say an airmass is located in the Canadian Prairie provinces. At any time of year this airmass will be relatively cold or cool in comparison to airmasses farther south, in the Great Plains for instance. It will also be rather dry, since there are no major bodies of water for this airmass to obtain water. This specific airmass is typical behind a cold front that we may encounter in the eastern two-thirds of the United States.
          A front is defined by the properties of the airmasses associated with it. However, another aspect of this definition involves which airmass is doing the pushing. There are five major types of fronts defined by this method. They are: cold front, warm front, occluded front, stationary front, and dry line.
          On a surface anaylsis, the fronts will be colored accoding to the image below (Figure 1.1).
          To define a front, think about what temperature and moisture parameters the airmasses around the front will have. It may be good to look at the surface observation plot to better define what kind of front you are dealing with (look at winds, temperatures, and dewpoints). Also, try to figure out which direction the front may be moving based on the surface winds.