Quantcast Advection Analysis

Order this information in Print

Order this information on CD-ROM

Download in PDF Format


Click here to make tpub.com your Home Page

Page Title: Advection Analysis
Back | Up | Next

tpub.com Updates




Information Categories
.... Administration
Food and Cooking
Nuclear Fundamentals
  Educational CD-ROM's
Printed Manuals
Downloadable Books


Back ] Home ] Up ] Next ]

Click here to Order your Radar Equipment Online

Advection Analysis

In meteorology, advection refers to the horizontal transport of heat or other properties. Advection charts, like thickness charts, are constructed between any two desired constant-pressure levels. In fact, they are usually constructed on thickness charts. Cold or warm air advection is indicated at the same intersections used to compute thickness. Advection arrows indicate the mean direction of flow in the layer. They are, for the most part, perpendicular to the thickness lines. Blue arrows indicate cold air advection and red arrows warm air advection. If the flow is such that it crosses thickness lines from higher height values to lower height values, the advection is warm; and from lower to higher values, it’s cold. The thumb rule to follow when constructing advection arrows is that when the contour of the lower pressure level is to the left looking downstream, advection is cold; but when it is to the right, advection is warm. See figure 8-1-13.

A derivative of the thermal wind equation and advection arrows is the thermal wind rule. It simply states that in the Northern Hemisphere if the wind backs with height, cold advection is indicated; and if the wind veers with height, warm air advection is indicated. Figure 8-1-14 illustrates the thermal wind rule as it applies in the Northern Hemisphere.

Time Differential Analysis

Time differential charts show the amount and direction of change of a meteorological quantity over a given period of time. They are used to track upper-height centers. They are usually drawn at 24-hour intervals, vice every 12 hours, to minimize diurnal effects.

Construction is as follows: Take two charts, 24 hours apart and of the same level, and lay the most recent over the other. Over these lay a clean acetate or blank chart. Using a light table, algebraically subtract the contour values of the most recent chart from those of the earlier chart. This is done where the contours of the two charts intersect. Lines are then constructed connecting like height differences. Falling height lines are drawn in red, rising heights in blue, and lines of no height change are drawn in purple. These lines are labeled in decimeters. The centers of rising

Figure 8-1-13.—Explanation of advection arrow construction.

Figure 8-1-14.—The thermal wind rule (Northern Hemisphere).

and falling heights are then transposed onto a blank chart (if acetate was used). These centers are then tracked in the same manner as are the pressure centers on constant-pressure charts. See figure 8-1-15 for an illustration of time differential construction.

Back ] Home ] Up ] Next ]


Privacy Statement - Press Release - Copyright Information. - Contact Us - Support Integrated Publishing

Integrated Publishing, Inc.