# Chapter 3: Weather Map. Station Model and Weather Maps Pressure as a Vertical Coordinate Constant Pressure Maps Cross Sections

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1 Chapter 3: Weather Map Station Model and Weather Maps Pressure as a Vertical Coordinate Constant Pressure Maps Cross Sections

2 Weather Maps Many variables are needed to described dweather conditions. Local weathers are affected by weather pattern. We need to see all the numbers describing weathers at many locations. We need weather maps. (from Understanding Weather & Climate) A picture is worth a thousand words.

3 The Station Model Meteorologists need a way to condense all the numbers describing the current weather at a location into a compact diagram that takes up as little space as possible on a weather map. (from Meteorology: Understanding the Atmosphere) This compressed geographical g weather report is called a station model.

4 Weather Map on 7/7/2005 (from Meteorology: Understanding the Atmosphere)

5 Isobar It is useful to examine horizontal pressure differences across space. Pressure maps depict isobars, lines of equal pressure. Through analysis of isobaric charts, pressure gradients are apparent. Steep (weak) pressure gradients are indicated by closely (widely) spaced isobars.

6 The Station Model: Cloudiness (from Meteorology: Understanding the Atmosphere)

7 The Station Model: Wind (Northeasterly wind) Wind speed is indicated to the right (left) side of the coming wind vector in the Northern (Southern) Hemisphere Wind speeds are indicated in units of knot. 1 international knot = 1 nautical mile per hour (exactly), = kilometer per hour (exactly), = meters per second, = miles per hour (approximately)

8 The Station Model: Pressure The pressure value shown is the measured atmospheric pressure adjusted to sea level. The units used are mb. To save space, the thousand and the hundred values, and the decimal point are dropped. So 138 means mb To decode the value of pressure on the station model, add a 9 if the firstnumberis678or9;otherwiseadda10 is 6, 7, 8, otherwise a 10.

9 Pressure Correction for Elevation Pressure decreases with height. Recording actual pressures may be misleading as a result. All recording stations are reduced to sea level pressure equivalents to facilitate horizontal comparisons. Near the surface, the pressure decreases about 100mb by moving 1km higher in elevation.

10 The Station Model: Pressure Tendency The change in surface pressure in the past three hours is plotted numerically and graphically on the lower right of the station model. The pressure rose and then fell over the past three hours, a total change of 0.3 mb.

11 The Station Model: Dew Point Temperature Dew point temperature (in united of ºF if reported in the US) indicates the moisture content. A higher value indicates a larger amount of moisture.

12 The Station Model: Significant Weather There are over a hundred d symbols for various weather conditions. If no symbol is plotted, no significant weather condition is occurring at tthe station. ti

13 Contour Lines on Weather Maps isotherm isobar isodrosotherm Meteorologists draw lines connecting points on weather maps with the same values of temperature (isotherm), pressure (isobar), dewpoint temperature (isodrosotherm), or other quantities to simply interpretation of data on the maps.

14 Pressure As a Vertical Coordinate Each altitude above a point on the Earth s surface has a unique value of pressure. Pressure can be easily substituted for altitude as a coordinate to specify locations in the vertical. Rawinsondes determine the height of the instrument above Earth s surface by measuring pressure. Because aircraft fly on constant pressure surfaces, upper air weather maps, first used extensively during World War II, traditionally i have been plotted on constant pressure surface. Fluid dynamics theories and equations that explain atmospheric motions are often in a more concise forms when they use pressure as a vertical coordinate.

15 Pressure Surface A pressure surface is a surface above the ground where the pressure has a specific value, such as 700mb. Constant pressure surfaces slope downward from the warm to the cold side. Since the atmosphere in the polar regions is cold and the tropical atmosphere is cold, all pressure surfaces in the troposphere slope downward from the tropics to the polar regions.

16 Height (Pressure) Map at a Constant Pressure (Height) At 500mb At 5700m Since the atmosphere in the polar regions is cold and the tropical atmosphere is warm, all pressure surfaces in the troposphere slope downward from the tropics to the polar regions. The pressure information on a constant altitude allow us to visualize where high- and low-pressure centers are located. The height information on a constant pressure surface convey the same information. The intensity of the pressure (or height) gradients allow us to infer the strength of the winds.

17 Upper-Level Weather Maps Meteorologists use height maps at constant pressure levels to describe weather conditions in the upper atmosphere. On constant pressure maps, we can infer a strong pressure gradient exists where a strong height gradient exists. Height maximum high pressure. Height minimum low pressure.

18 Station Model in Upper-Level Weather Maps Upper-Level Station Model Decameter = a metric unit of length equal lto 10 meters. Surface Station Model

19 Other Upper-Level Weather Maps 850mb: to identify fronts 700mb: intersects many clouds; moisture information is important 500mb: used to determine the location of short waves and long waves associated with the ridges and troughs in the flow pattern. Meteorologists examine vorticity (i.e. rotation of air) on this pressure level. 300, 250, and 200mb: near the top of the troposphere or the lower stratosphere; these maps are used to identify the location of jetsreams that steer the movements of mid-latitude storms.

20 Example: A 850mb Weather Map Stations whose pressure are less than (i.e. above) 850mb The 850mb map is particularly useful to identify the location of fronts. In this example, a low-level jet is seen flowing parallel to the cold front extending from New Mexico to Wisconsin.

21 Example: A 300mb Weather Map j jetstreaks i t h isotachs The 850mb map is particularly useful to identify the location of jetsreams. In this example, a jetstream flows northeastward from the west cost of the US, into the Great Lakes, and to the Atlantic Coast of Canada. Prof. JinJin-Yi Yu

22 Example: 500mb Weather Map The 500mb surface, which is in the center of the troposphere, is typically the altitude meteorologists use to examine vorticity pattern.

23 Vorticity Vorticity is the tendency for elements of the fluid to "spin spin.. Vorticity can be related to the amount of circulation or "rotation" "(or more strictly, the local langular rate of rotation) in a fluid. Definition: Absolute Vorticity Relative Vorticity

24 Three Sources of Vorticity

25 Vorticity-Related Flow Patterns Shear Vorticity Curvature Vorticity Even straight-line motion may have vorticity if the speed changes normal to the flow axis. (a) 300mb isotachs; (b) 300mb geopotential hights

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