1. Introduction to the basics of map analysis, the rules for drawing isolines, the rules for the analysis of equality, the basic analysis on the surface map, the analysis of isobars, the analysis of isotherms, as well as the definition of pressure patterns, the atmospheric elevation, the dent, the depression, the furrow, the recession zone , wavy barometric pattern, secondary depression, isothermal analysis, barometric isobaric analysis2. Introducing the characteristics and analysis of upper atmosphere maps (fixed pressure levels). Barometric Map Analysis 1000 mbar, Barometric Map Analysis 850 mbar, Barometric Map Analysis 700 mbar, Barometric Map Analysis 500 mbar, Barometric Map Analysis 300/250/200 mbar,3. Familiarity with preparing thickness maps, forming a thickness map, calculating the thickness directly on the thickness map, calculating the thickness by subtracting two pressure levels from each other, the characteristics of the thickness of the layer 1000-500 mbar, places of change of furrows and forecasts, furrows and heat emission at different levels,4. Being able to analyze the difference in dew point and wind analysis. Also revealing the compatibility between the surface map and the upper atmosphere map. In terms of changing the places of heights, depressions, grooves and indentations with height, identifying air fronts in the three dimensions.
Intended learning outcomes
a. Knowledge and understanding:A.1 The student will be familiar with the basics of map analysis and the rules for drawing equal lines for atmospheric elements.A.2 The student explains the method of drawing and analyzing upper atmosphere maps (fixed pressure levels).A.3 The student explains what a fish chart is, the requirements for a fish chart, how to prepare a fish chart.A.4 That the student explain the link between the changes that occur on the surface map and the changes that occur on the map of the upper atmosphere.B. Mental skills:B.1 The student analyzes the surface weather map by drawing isobars, isotherms, analyzing isobars and other atmospheric variables.B.2 That the student relates between the weather changes that occur on the 1000 millibar pressure level map and the changes that occur on the rest of the upper atmosphere maps.B.3 That the student derive the method of calculating the thickness graphically using the two maps of the upper atmosphere 1000 millibars and 500 millibars.B.4 The student should distinguish between a depression and a depression, and a depression and a gully.c. Practical and professional skills:C.1 That the student distinguish between the different pressure patterns over the surface map, such as: atmospheric elevation, bulge, depression, furrow, slump zone, wavy pressure pattern, and others.C. 2 That the student perform repeated exercises in the process of analyzing the upper air maps (850 mbar, 700 mbar, 500 mbar).C.3 That the student diagnoses the atmospheric situation using the thickness map by linking the heating state with an increase in thickness and the cooling state with a decrease in thickness.C.4 The student should use special programs for analyzing winds using the common method called the Wind Rose.Dr.. General and transferable skills:D.1 The student should be able to use computer programs to help analyze surface maps and upper atmosphere maps in the required manner.D.2 The student should be able to actively participate in the activities related to the practical course by repeating exercises on drawing isobars, temperature, barometric slope, and others.D.3 The student should be able to use modern technology to help analyze the pressure levels map of 300, 250, 200 millibars.D.4 The student should be able to work in a team under the supervision of the course instructor, especially when identifying air fronts on the weather map.
