USING A MATHEMATICAL APPROACH TO DETERMINE

VORTICITY ADVECTION (TERM B)


Obtain an image of the 500-hPa wind barb plan view and wind direction at the location diamond by following these steps:


1) In the “Displays” menu, check the box next to “Wind Barbs” under the section labeled “WIND PLOTS.”

2) Under the section titled “DRAWING TOOLS” in the “Displays” menu, check the box next to “Geostrophic Wind Vector.”



Q9 - What two forces are in balance in “geostrophic” flow?  Is the flow at 500 hPa approximately geostrophic?  How can you tell?

Q10 - From the wind bards, what is the approximate 500-hPa wind speed (in knots) at the location diamond?  Convert this rough estimate to m/s.


3) Uncheck the boxes next to “Wind Barbs” under “WIND PLOTS” and “Geostrophic Wind Vector” under “DRAWING TOOLS.”

4) Also, uncheck the box corresponding to “500 hPa Geopotential Height Contours” in the “GEOPOTENTIAL HEIGHT PLOTS” section of the “Displays” menu.  This should yield a blank map once again with only the gray location diamond fixed in western Virginia.


Obtain the following image of the 500-hPa absolute vorticity gradient at the location diamond by following these steps:


1) Under the main heading titled “ABSOLUTE VORTICITY PLOTS.”  Check the following subcategories:

                   a) “500 hPa Absolute Vorticity Contours (Max)”

                   b) “500 hPa Colored Absolute Vorticity Max”

                   c) “500 hPa Absolute Vorticity Contours (Diamond)”

2) In addition, check the boxes corresponding to “Gradient of Absolute Vorticity” and “Range and Bearing” under the “DRAWING TOOLS” section of the “Displays” menu.



Q11 - What is the mathematical definition of a gradient?  Why is the pink vector (absolute vorticity gradient) directed to the WNW?

Q12 - What is the value of the contour of absolute vorticity at the left end of the range and bearing tool overlapping the pink gradient vector?  Note that the value of the 500-hPa absolute vorticity at the location diamond is 12 x 10-5 s-1.  From the computed “Distance” appearing under the “Range and Bearing” label in the “Displays” menu and the previously interpreted values of vorticity, calculate a rough estimate of the magnitude of the gradient of absolute vorticity at the location diamond.


3) Uncheck the box next to “ABSOLUTE VORTICITY PLOTS” and “Range and Bearing” under “DRAWING TOOLS.”  Leave the box corresponding to “Gradient of Absolute Vorticity” checked.


Obtain an image of the angle between the gradient of absolute vorticity and the geostrophic wind vector by simply checking the box next to “Geostrophic Wind Vector” under the “DRAWING TOOLS” section of the “Displays” menu.



Q13 - What is the approximate angle between the vectors?


Remove the vectors from the display by unchecking the box corresponding to each under the “DRAWING TOOLS” section of the “Displays” menu.


Q14 - Recall that Term B in the Q-G height tendency equation is given by .  Using the definition of a dot product, Term B can be rewritten in the following form:  .  Use your estimates of  (magnitude of the geostrophic wind),  (magnitude of the absolute vorticity gradient), and  (estimated angle between the geostrophic wind vector and the gradient of absolute vorticity), and an accepted value of  to compute an estimated total value, , of Term B.

Q15 - Ignoring Term C, note from the Q-G height tendency equation that .  From the procedures followed in the answer to Q14, it is clear that this can be rewritten as .  So, based on your computation of , use the relationship between  and  to predict either a height fall or a height rise.


ANSWERS TO QUESTIONS



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