Vietnam: What are xem bóng đá trực tiếp vtv2 guidelines for xem bóng đá trực tiếp vtv2 analysis of factors that affect rainfall? What learning outcomes are required for 10th-grade students regarding xem bóng đá trực tiếp vtv2 atmospheric content in xem bóng đá trực tiếp vtv2 Geography curriculum?
What are xem bóng đá trực tiếp vtv2 guidelines for xem bóng đá trực tiếp vtv2 What are xem bóng đá trực tiếp vtv2 guidelines for xem bóng đá trực tiếp vtv2 analysis of factors that affect rainfall?
Rainfall is an essential climatic factor that determines xem bóng đá trực tiếp vtv2 distribution of water on xem bóng đá trực tiếp vtv2 Earth's surface, directly affecting living environments, ecosystems, and human economic activities. Rainfall is not evenly distributed across areas andaffected by numerous factors such as air pressure, fronts, wind, ocean currents, and terrain.
Students may refer to xem bóng đá trực tiếp vtv2 followingguidelines for theanalysis offactors that affectrainfall:
| 1. Air Pressure - Low Pressure Area: This is where air is drawn upwards, cooled, condensed, forming clouds, leading to rain. Low pressure areas generally have high rainfall, typical of xem bóng đá trực tiếp vtv2 equatorial region. - High Pressure Area: Here, air is compressed, unable to ascend to form clouds, resulting in little or no rain. Areas such as xem bóng đá trực tiếp vtv2 polar regions and xem bóng đá trực tiếp vtv2 tropics are examples of this phenomenon. 2. Fronts - A front is xem bóng đá trực tiếp vtv2 boundary between two masses of air with different temperatures and characteristics. When warm air rises over cold air at fronts, intense moisture condensation occurs, causing rain. - Regions with warm fronts, cold fronts, or tropical convergence zones often have frequent heavy rains. For example, xem bóng đá trực tiếp vtv2 tropical convergence area in xem bóng đá trực tiếp vtv2 East Sea usually experiences prolonged heavy rain. 3. Wind - Ocean Wind: Coastal areas or regions receiving winds from xem bóng đá trực tiếp vtv2 ocean usually have high rainfall due to evaporation from xem bóng đá trực tiếp vtv2 sea. - Inland Areas: Regions without moisture-bearing winds from xem bóng đá trực tiếp vtv2 sea are usually less rainy, sometimes even deserts. - Monsoon: Areas with active monsoons (such as Southeast Asia) usually have heavy rains during xem bóng đá trực tiếp vtv2 moist monsoon from xem bóng đá trực tiếp vtv2 ocean. - Trade Winds: Areas with strong trade winds are often arid with little rainfall. 4. Ocean Currents - Warm Ocean Currents: When warm currents flow along xem bóng đá trực tiếp vtv2 coast, xem bóng đá trực tiếp vtv2 increased temperature causes more evaporation, leading to heavy rain. For example, coastal areas affected by xem bóng đá trực tiếp vtv2 Gulf Stream in xem bóng đá trực tiếp vtv2 Atlantic. - Cold Ocean Currents: In coastal regions with cold currents, moisture condenses before reaching xem bóng đá trực tiếp vtv2 shore, leading to aridity. For example, xem bóng đá trực tiếp vtv2 Atacama Desert on xem bóng đá trực tiếp vtv2 Pacific coast, affected by xem bóng đá trực tiếp vtv2 Humboldt Current. 5. Terrain - Elevation: In areas with high terrain, air moving upwards cools, causing moisture to condense, leading to rain. However, beyond a certain height, xem bóng đá trực tiếp vtv2 air becomes dry and rainless. - Windward and Leeward Slope: + Windward Slope (main wind direction carrying moisture): High rainfall due to moist air rising, cooling, and condensing. + Leeward Slope: Less rain or dry conditions as xem bóng đá trực tiếp vtv2 air loses most moisture after crossing xem bóng đá trực tiếp vtv2 windward slope. 6. Conclusion Rainfall in an area results from a combined effect of natural factors such as air pressure, fronts, wind, ocean currents, and terrain. These factors don't operate independently but often coordinate, causing uneven distribution of rainfall on xem bóng đá trực tiếp vtv2 Earth's surface. Understanding these factors not only helps explain climatic phenomena but also aids in water resource management and effective weather forecasting. |
Note: xem bóng đá trực tiếp vtv2 content is for reference only.
What are xem bóng đá trực tiếp vtv2 guidelines for xem bóng đá trực tiếp vtv2 analysis of factors that affect rainfall? What learning outcomes are required for 10th-grade students in Vietnam regarding xem bóng đá trực tiếp vtv2 atmospheric content in xem bóng đá trực tiếp vtv2 Geography curriculum? (Image from Internet)
What learning outcomes are required for10th-grade students in Vietnam regardingthe atmospheric content in theGeography curriculum?
According to Section 5 of xem bóng đá trực tiếp vtv2 General education program in Geography issued along withCircular 32/2018/TT-BGDDT, xem bóng đá trực tiếp vtv2 learning outcomes required for10th-grade students in Vietnam regardingthe atmospheric content in theGeography curriculum are as follows:
- Define xem bóng đá trực tiếp vtv2 concept of atmosphere.
- Present xem bóng đá trực tiếp vtv2 distribution of air temperature on Earth by geographic latitude; continents, oceans; terrain.
- Present xem bóng đá trực tiếp vtv2 formation of air pressure belts on Earth, reasons for changes in air pressure.
- Present several main wind types on Earth; some local wind types.
- Analyze factors affecting rainfall and present its global distribution.
- Analyze data tables, diagrams, maps, and sketches of several atmospheric elements (temperature, air pressure, wind, rain).
- Read climate zone maps on Earth; analyze some climate diagrams.
- Explain some weather and climate phenomena in reality.
How many assessment levels for training results of 10th-grade students in xem bóng đá trực tiếp vtv2 entire school year in Vietnam are there?
Under Point b, Clause 2, Article 8 ofCircular 22/2021/TT-BGDDT, xem bóng đá trực tiếp vtv2 training results of 10th-grade students in xem bóng đá trực tiếp vtv2 entire school year in Vietnam are assessedat four levels:
-Excellent: a student is placed in Excellent category in xem bóng đá trực tiếp vtv2 2ndsemester and in Good category or higher in xem bóng đá trực tiếp vtv2 1stsemester.
-Good: a student is placed in Good category in xem bóng đá trực tiếp vtv2 2ndsemester and Qualified category or higher in xem bóng đá trực tiếp vtv2 1st semester; or Qualified category in xem bóng đá trực tiếp vtv2 2ndsemester and Good category in xem bóng đá trực tiếp vtv2 1stsemester; or Good category in xem bóng đá trực tiếp vtv2 2ndsemester and Qualified category or Unqualified category in xem bóng đá trực tiếp vtv2 1stsemester.
-Qualified: a student is placed in Qualified category in xem bóng đá trực tiếp vtv2 2ndsemester and Good, Qualified, or Unqualified category in xem bóng đá trực tiếp vtv2 1stcategory; or Good category in xem bóng đá trực tiếp vtv2 2ndsemester and Unqualified in xem bóng đá trực tiếp vtv2 1stsemester.
-Unqualified: other cases.
