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<br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br /> <br />GLOSSARY <br /> <br />Advection: The process of transfer (of an air mass property) by virtue of motion. In particular <br />cases, advection may be confined to either the horizontal or vertical components of the motion. <br />However, the term is often used to signifY horizontal transfer only. <br /> <br />Air mass: Extensive body of air approximating horizontal homogeneity, identified as to source <br />region and subsequent modifications. <br /> <br />Barrier: A mountain range that partially blocks the flow of warm humid air from a source of <br />moisture to the basin under study. <br /> <br />Basin shape: The physical outline of the basin as determined from topographic charts or field <br />survey. <br /> <br />Cold front: Front where relatively colder air displaces warmer air. <br /> <br />Convective rain: Rainfall caused by the vertical motion of an ascending mass of air that is <br />warmer than the environment and typically forms a cumulonimbus cloud. The horizontal <br />dimension of such a mass of air is generally of the order of 12 miles or less. Convective rain is <br />typically of greater intensity than either of the other two main classes of rainfall (cyclonic and <br />orographic) and is often accompanied by thunder. The term is more particularly used for those <br />cases in which the precipitation covers a large area as a result of the agglomeration of <br />cumulonimbus masses, <br /> <br />Convergence: Horizontal shrinking and vertical stretching ofa volume of air, accompanied by <br />net inflow horizontally and internal upward motion. <br /> <br />Cooperative station: The location of a weather observation site where an unpaid observer <br />maintains a climatological station for the National Weather Service. <br /> <br />Cyclone: A distribution of atmospheric pressure in which there is a low central pressure relative <br />to the surroundings. On large-scale weather charts, cyclones are characterized by a system of <br />closed constant pressure lines (isobars), generally approximately circular or oval in form, <br />enclosing a central low-pressure area. Cyclonic circulation is counterclockwise in the northern <br />hemisphere and clockwise in the southern. (That is, the sense of rotation about the local vertical <br />is the same as that of the earth's rotation,) <br /> <br />Dewpoint: The temperature to which a given parcel of air must be cooled at constant pressure <br />and constant water vapor content in order for saturation to occur. <br /> <br />xvii <br />