Weather Station Model

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Fun with Weather Maps! (no, really stop laughing) AOSC 200 Tim Canty Class Web Site: http://www.atmos.umd.edu/~tcanty/aosc200 Topics for today: Station Model Temperature Maps Pressure Maps Fronts Lecture 03 Sept 4 2018 1 Weather Station Model Fig 1-17 Meteorology: Understanding the Atmosphere 2

Weather Station Model The weather station model tells you what the conditions are like at the surface Fig 2-1-1 Weather: A Concise Introduction 3 Weather Station Model The central circle indicates cloud cover Fig 2-1-2 Weather: A Concise Introduction 4

Weather Station Model The symbol located between the air temperature and dew point temperature indicates significant weather Fig 2-1-3 Weather: A Concise Introduction 5 Weather Station Model The line indicates the direction the wind is coming from (in this case from the Northeast) and the barbs and pennants indicate wind speed Fig 2-1-4 Weather: A Concise Introduction 6

Weather Station Model The line indicates the direction the wind is coming from (in this case from the Northeast) and the barbs and pennants indicate wind speed Fig 2-1-5 Weather: A Concise Introduction 7 Weather Station Model Reading the pressure can be a little confusing. In the figure above, the pressure is 987 hpa (mbar) at the surface Fig 2-1-1 Weather: A Concise Introduction 8

Today s Weather Map http://www.wpc.ncep.noaa.gov/sfc/namussfcwbg.gif 9 Temperature Maps Temperature maps are often colored based on how warm (red) or cold (blue) the surface temperatures are Fig 2-2 Weather: A Concise Introduction 10

Temperature Maps The black lines indicate isotherms or lines of constant temperature. These maps help us identify the air masses that are controlling surface conditions and the temperature frontal boundaries between them Fig 2-2 Weather: A Concise Introduction 11 Temperature Fronts A cold front is a region where cold air is replacing warm air. It s indicated by a blue line with blue triangles pointing in the direction the air mass is moving. Fig 2-3 Weather: A Concise Introduction 12

Temperature Fronts A warm front is a region where warm air is replacing cold air. It s indicated by a red line with red half circles pointing in the direction the air mass is moving. Fig 2-3 Weather: A Concise Introduction 13 Temperature Fronts Recognize the fronts by the symbols!!! You might have a black and white map (like on a test.hint hint!!) and can t rely on the colors to tell you which type of front you re looking at. Fig 2-3 Weather: A Concise Introduction 14

Pressure Maps The black lines indicate isobars or lines of constant pressure. These maps help us identify regions of high pressure ( H ) and low pressure ( L ). They also give some indication of surface wind speed and direction. Fig 2-4 Weather: A Concise Introduction 15 Pressure Maps Generally, isobars are plotted at 4 hpa intervals If it helps, consider this like a map of surface height and you ll get an idea of where are is flowing too and how fast it s moving. Fig 2-4 Weather: A Concise Introduction 16

Pressure Maps Closed contours define regions of high pressure and low pressure. Fig 2-5 Weather: A Concise Introduction 17 Pressure Maps Isobars that aren t closed can still help us define regions of increasing ( ridges ) and decreasing ( troughs ) pressure. Fig 2-6 Weather: A Concise Introduction 18

Temperature Maps We can combine the different ways of looking at surface data to create what you may recognize as a modern weather map Fig 2-2 Weather: A Concise Introduction 19 Weather Maps We can combine the different ways of looking at surface data to create what you may recognize as a modern weather map Fig 2-2 Weather: A Concise Introduction 20

Upper Level Maps We can look at pressure maps at a some particular altitude but the mathematics becomes very complicated Instead, we look at altitude of a specific pressure level. The figures to the right show the height (in meters) of the 850 hpa surface. Fig 2-8 Weather: A Concise Introduction 21 Upper Level Maps The station model provides slightly different information than at the surface. The height of the pressure surface is in the position where pressure used to be. Maps of this information are called isobaric maps Fig 2-9 Weather: A Concise Introduction 22

Weather Maps: Surface We can combine the different ways of looking at surface data to create what you may recognize as a modern weather map Fig 2-2 Weather: A Concise Introduction 23 Weather Maps: 500 mb The color contours represent wind speed (in knots). Notice that the fastest winds in the central US are almost above the position of the surface low pressure. Here the black lines are in decameters. Fig 2-10 Weather: A Concise Introduction 24

Weather Maps: 500 mb The height of the layer can indicate surface temperatures. Why? Fig 2-10 Weather: A Concise Introduction 25 Weather Maps: 500 mb Sometimes this information is plotted as the 1000-500 hpa thickness Fig 2-10 Weather: A Concise Introduction 26

Prognostic Charts Fig 9.5: Essentials of Meteorology 27 Prognostic Charts Fig 9.5: Essentials of Meteorology 28

Prognostic Charts Fig 9.5: Essentials of Meteorology 29 Prognostic Charts Fig 9.5: Essentials of Meteorology 30