|
Evaluation Number |
Evaluation methods |
Duration of evaluation |
Evaluation Weight |
Percentage |
Date of evaluation (week) |
Feedback |
|
First evaluation |
First half exam |
One and a half hours |
Section 1. 5 |
25 % |
Week 6 |
- |
|
Second evaluation |
Second Half Exam |
One and a half hours |
Section 6. 10 |
25 % |
Week 11 |
- |
|
Final Evaluation |
Final exam |
2 hours |
All Rapporteur |
50 % |
According to the final exam schedule |
- |
|
total |
100 degrees |
100% |
|
|
||
:(References)
|
Reference Address |
Publisher |
Version |
Author |
Whereabouts |
|
Meteorological |
Book House - Egypt |
2nd edition |
Dr. Mohamed Ahmed AL sied |
Section Library |
|
Atmospheric Science |
Academic Press, Inc. USA, 1977 |
1st edition |
John M. Wallace Peter V. Hobbs |
University Sales |
|
General Meteorology |
Academic Press, Inc. USA, 1983 |
4th edition |
Bayers |
Section Library |
Course contents:
|
Week |
Scientific topic |
Number of hours |
Lecture |
Exercises |
Independent Memory |
|
1. |
Meteorology, primary branches - branche The applied. |
8 |
2 |
2 |
4 |
|
2. |
The atmosphere - its properties, its components, its composition - layers of the atmosphere. |
8 |
2 |
2 |
4 |
|
3. |
Air Density-Calculating air density, changing air density at Earth's surface, changing air density with height. atmospheric pressure - change between atmospheric pressure and air weight, atmospheric pressure units, |
8 |
2 |
2 |
4 |
|
4. |
Daily change of atmospheric pressure, the effect of temperature on decreasing atmospheric pressure with height. |
8 |
2 |
2 |
4 |
|
5. |
Thermal equilibrium of the atmosphere and temperature distribution-heat sources, air temperature at the earth's surface, |
8 |
2 |
2 |
4 |
|
6. |
The difference of temperature at the Earth's surface between land and water, the effect of the cloud on the temperature at the Earth's surface, the daily change of air temperature |
8 |
2 |
2 |
4 |
|
7. |
The extent of daily temperature change, the rate of thermal attrition in the air, and the daily change in the rate of thermal attrition. |
8 |
2 |
2 |
4 |
|
8. |
Water vapor in Jo-properties and the effect of water vapor in the atmosphere-pressure water vapor, the effect of water vapor on air density, air saturation with water vapor, relative humidity, |
8 |
2 |
2 |
4 |
|
9. |
Dew Point Temperature, Mixing Ratio, Water Vapor Intensifies in Jo-Mahe, Condensation Intentions, Water Droplets Over Cooled |
8 |
2 |
2 |
4 |
|
10. |
Conditioning conditions of water vapour in the jet - air cooling by conduction, air cooling by blending, air self-cooling, dry self-attrition rate, saturated self-attrition rate, precipitation. |
8 |
2 |
2 |
4 |
|
11. |
Stability and instability in the atmosphere - general theory of stability, stability in the atmosphere |
8 |
2 |
2 |
4 |
|
12. |
Stability and thermal attrition rate of the prevailing atmosphere, dry self-attrition rate, saturated self-attrition rate, general rules of stability and instability in the atmosphere, weather conditions that accompany stability and instability in the atmosphere. |
8 |
2 |
2 |
4 |
|
13. |
Wind-Wind Geostrovic, Wind Downhill |
8 |
2 |
2 |
4 |
|
14. |
Fog-types fog, the effect of fog on vision |
8 |
2 |
2 |
4 |
