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Contouring and Map Analysis Lecture 2 February 4, 2010.

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1 Contouring and Map Analysis Lecture 2 February 4, 2010

2 Today’s Agenda  Attendance  Weather Discussion  New material  In class activity

3 Contouring Station models do a good job of telling us what the weather conditions are like over a large area or at one station at one time…Station models do a good job of telling us what the weather conditions are like over a large area or at one station at one time… But contouring gives us even more informationBut contouring gives us even more information Contoured maps give easy-to-read, general information about small to large areasContoured maps give easy-to-read, general information about small to large areas Contoured maps help in easily diagnosing and depicting weather features and variablesContoured maps help in easily diagnosing and depicting weather features and variables

4 Contour analysis is vital in:  Finding the location of atmospheric and oceanic fronts.  Locating regions with the potential of severe weather  Tracking storms, such as hurricanes and blizzards  Tracking the movement of pollutants

5  A contour line is a line of a constant value or an isopleth. Where iso means same and pleth means value.  A contour analysis involves drawing multiple isopleths.  Depending on what you are contouring, the lines have different names

6 What can you contour?  Isobar: A line of constant pressure  Isoheight: A line of constant height  Isotherm: A line of constant temperature  Isodrosotherm: A line of constant dewpoint  Isotach: A line of constant wind speed  Isohyet: A line of constant precipitation accumulation  Isoneph: A line of constant cloudiness  Isohaline: A line of constant salinity (saltiness in the ocean)

7 Isobars and Isoheights

8 Isotherms and Isoheights at 850mb

9 Rules and Tips for Contouring  Contours will never cross each other  Contours never branch or fork, they are always one continuous line  Do not create contours where there is no data (i.e., over the oceans)  Always label your contours  Contour at evenly spaced increments (for surface temperature, we’ll do every 5 degrees Fahrenheit, and for sea level pressure, every 4 millibars)

10 Rules and Tips for Contouring  Use a pencil! You will be erasing…  Locate regions of high and low values first  Initially, sketch out how you will be making your first few contours  Make your lines as smooth as possible.  Ignore outliers, data that doesn’t seem like it fits with the “big picture.”  If you need more help, try: tutorial on web

11 Helpful Hint  Think about the contour as a line separating the observations with higher values on one side of the line, and lower values on the other side: 19 20 21 17 21 23 24 19 29 24 30 29 25 24 27 22 30 Draw the 25-line:

12 Helpful Hint  Think about the contour as a line separating the observations with higher values on one side of the line, and lower values on the other side: 19 20 21 17 21 23 24 19 29 24 30 29 25 24 27 22 30 Draw the 25-line:

13 Helpful Hint  Think about the contour as a line separating the observations with higher values on one side of the line, and lower values on the other side: 19 20 21 17 21 23 24 19 29 24 30 29 25 24 27 22 30 Draw the 25-line: 25

14 Examples  Say these observations are temperatures. Where should we draw the 15 o F isotherm??

15 Examples

16 Examples Say these observations are temperatures. Where should we draw the 75 o F and 80 o F isotherms??

17 Examples

18 Want extra practice? Professor Steve Ackerman has developed a website which allows you to practice contour analysis through a Java-applet: http://profhorn.meteor.wisc.edu/wxwise/contour/contour1.html

19 In Class Assignment

20 To convert from Z time to CST, subtract 6 hours. 05Z = 11 PM CST

21 1020 1008


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