weather analysis pg. 81. recording data after weather data is collected it is plotted on a map using...
DESCRIPTION
Surface Analysis to plot data globally, use isopleths lines that connect points of equal values lines of equal pressure-isobars lines of equal temps- isotherms the spacing of lines can provide info wind- the closer the lines the faster pressure- closers the isobars, larger the pressure difference; strong winds to plot data globally, use isopleths lines that connect points of equal values lines of equal pressure-isobars lines of equal temps- isotherms the spacing of lines can provide info wind- the closer the lines the faster pressure- closers the isobars, larger the pressure difference; strong windsTRANSCRIPT
Weather Analysispg. 81
Recording dataafter weather data is collected it is plotted on a map using station modelsstation models- record of weather data for a particular site at a particular timegives meteorologists a uniform way to communicate data
Surface Analysis
to plot data globally, use isopleths
lines that connect points of equal values
lines of equal pressure-isobars
lines of equal temps- isotherms
the spacing of lines can provide info
wind- the closer the lines the faster
pressure- closers the isobars, larger the pressure difference; strong winds
isopleths
can show where high and low pressure systems arecombined with isotherms it will tell the frontal system theremust know current weather conditions before forecasting can occur
isopleth
Short Term Forecast
reliable forecasts must be taken from data at multiple levels in the atmospherecan be digital or analog forecastsBased on the fact that the atmosphere behaves as a fluid
digital forecasts
can use mathematical equations to determine how variables change with time (temp, pressure, density)forecasts that rely on mathematical data are digital forecaststhe more data, the more accurate the forecast
analog forecastscompares current weather patterns to patterns that have happened in the pastassumes weather systems behave in a similar fashionmust find a past event that is similar in all levels of the atmosphereuseful for monthly and seasonal forecasting
long term forecasting
factors in the landscape make it hard to accurately predict weatherforecasts that are in the 1-3 day range are no longer based on the movement of clouds and precipitationdependent on the upper level features such as low pressure systemscan accurately predict if it will be wet or dry and when rain will come
Accuracy in long term forecasting
4-7 day forecasts rely on changes in the surface weather based on weather patterns in the troposphere and lower stratospherecan only estimate weathermust be able to understand how all facets effect weather patterns for future
Station modelpg.82
• Create a station model for our weather today. Include the following (use appendix E pg. 915):• Type of low cloud• Temperature• Wind direction and speed• Dew point temp• Percentage of sky covered• Barometric pressure
• Turn in: Ch. 12 assessment pg. 326-327• #’s 1-6, 8-19• #’s 1-5 test practice