What is đá bóng trực tiếp direction of đá bóng trực tiếp prevailing wind in Vietnam during đá bóng trực tiếp summer season? What are regulations on evaluation by scores for continuing education students at lower secondary level in Vietnam?
What is đá bóng trực tiếp direction of đá bóng trực tiếp prevailing wind in Vietnam during đá bóng trực tiếp summer season?
During đá bóng trực tiếp summer, due to geographical position and changes in air pressure, our country is primarily influenced by đá bóng trực tiếp southwest monsoon, including đá bóng trực tiếp particularly distinctive southern foehn wind (Laos wind). These winds bring distinct characteristics in terms of direction and nature, contributing to đá bóng trực tiếp formation of đá bóng trực tiếp rainy season and various weather phenomena across regions.
1. Southwest Monsoon
- Wind Direction: đá bóng trực tiếp wind blows from đá bóng trực tiếp southwest direction.
- Origin: đá bóng trực tiếp southwest monsoon forms from đá bóng trực tiếp high-pressure area over đá bóng trực tiếp Indian Ocean and its surrounding seas (primarily đá bóng trực tiếp Bay of Bengal) blowing towards đá bóng trực tiếp tropical low-pressure area over đá bóng trực tiếp Asian continent.
- Characteristics:
+ đá bóng trực tiếp southwest monsoon carries moisture from đá bóng trực tiếp Indian Ocean and đá bóng trực tiếp Bay of Bengal. When it reaches Vietnam through đá bóng trực tiếp Gulf of Thailand and đá bóng trực tiếp East Sea, it causes significant rainfall, especially in đá bóng trực tiếp South, Central Highlands, and parts of đá bóng trực tiếp Central region.
+ It is đá bóng trực tiếp main cause of đá bóng trực tiếp rainy season in these areas, particularly in đá bóng trực tiếp Central Highlands, providing abundant water resources for agricultural production and daily life.
+ đá bóng trực tiếp southwest monsoon typically prevails from May to October, resulting in continuous heavy rains in đá bóng trực tiếp South and Central Highlands.
2. Southern Foehn Wind (Laos Wind)
- Wind Direction: Also primarily southwest.
- Origin: đá bóng trực tiếp southwest wind from đá bóng trực tiếp Indian Ocean blows through đá bóng trực tiếp Bay of Bengal and Laos before crossing đá bóng trực tiếp Truong Son Mountains to reach Vietnam.
- Formation Process:
+ As đá bóng trực tiếp southwest wind blows over đá bóng trực tiếp Truong Son Mountains, its moisture is retained on đá bóng trực tiếp western side of đá bóng trực tiếp mountains (đá bóng trực tiếp territory of Laos). Consequently, đá bóng trực tiếp air becomes dryer and hotter after crossing đá bóng trực tiếp mountain peaks to reach Central Vietnam.
- Characteristics:
+ đá bóng trực tiếp southern foehn wind causes severe drought and extreme heat in đá bóng trực tiếp North Central Coast and Central coastal provinces like Thanh Hoa, Nghe An, Ha Tinh, Quang Binh, Quang Tri, Thua Thien - Hue.
+ This wind typically occurs from May to July, sometimes extending into August, subjecting đá bóng trực tiếp region to harsh heat, drought, and water shortages, hindering agricultural production as well as daily activities.
Explanation of đá bóng trực tiếp Prevalence of Southwest Wind in Summer
- Influence of low and high pressure:
+ In summer, when đá bóng trực tiếp sun shines most intensely in đá bóng trực tiếp Northern Hemisphere, đá bóng trực tiếp Asian continent (especially Southeast Asia) heats up significantly, forming a large low-pressure area.
+ Meanwhile, đá bóng trực tiếp Indian Ocean, Bay of Bengal, and East Sea maintain high-pressure areas. This pressure difference creates a wind flow from đá bóng trực tiếp high-pressure area of đá bóng trực tiếp Indian Ocean to đá bóng trực tiếp low-pressure area over đá bóng trực tiếp Asian continent and Vietnam.
+ Southeast Asia Monsoon System: Vietnam is located in đá bóng trực tiếp area influenced by đá bóng trực tiếp Southeast Asia monsoon. In summer, đá bóng trực tiếp southwest monsoon from đá bóng trực tiếp Indian Ocean combines with air masses from đá bóng trực tiếp East Sea, creating đá bóng trực tiếp prevailing wind during this period.
+ đá bóng trực tiếp role of đá bóng trực tiếp Truong Son Mountains: đá bóng trực tiếp Truong Son Mountains act as a barrier and alter đá bóng trực tiếp characteristics of đá bóng trực tiếp southwest winds. As they cross đá bóng trực tiếp mountains, these winds lose moisture and become dry and hot, causing đá bóng trực tiếp foehn effect in đá bóng trực tiếp North Central Coast and Central regions.
Impact of đá bóng trực tiếp Southwest Monsoon and Southern Foehn Wind
- Southwest Monsoon:
+ It brings substantial rainfall to đá bóng trực tiếp South and Central Highlands, helping to replenish water resources for agricultural production, irrigation, and hydroelectric development.
+ Plays a crucial role in forming đá bóng trực tiếp rainy season, helping to alleviate đá bóng trực tiếp heat in đá bóng trực tiếp southern region.
- Southern Foehn Wind (Laos Wind):
+ Causes arid conditions, extreme heat in đá bóng trực tiếp North Central Coast and Central coastal regions, increasing đá bóng trực tiếp risk of forest fires, droughts, and adversely affecting crops.
+ At đá bóng trực tiếp same time, đá bóng trực tiếp hot dry weather also increases đá bóng trực tiếp demand for water in daily and production activities, placing significant pressure on water resources in this area.
Conclusion
Thus, đá bóng trực tiếp prevailing winds in Vietnam during đá bóng trực tiếp summer are đá bóng trực tiếp southwest monsoon and đá bóng trực tiếp southern foehn wind. đá bóng trực tiếp southwest monsoon brings heavy rains, cooling temperatures, and nourishing crops in đá bóng trực tiếp South and Central Highlands, while đá bóng trực tiếp southern foehn wind (Lao Wind) causes severe dryness in đá bóng trực tiếp Central region. đá bóng trực tiếp presence of these winds not only reflects đá bóng trực tiếp tropical monsoon climate characteristics of Vietnam but also greatly impacts đá bóng trực tiếp life, production, and activities of đá bóng trực tiếp population.
Note: đá bóng trực tiếp contentis for reference purposes only.
What is đá bóng trực tiếp direction of đá bóng trực tiếp prevailing wind in Vietnam during đá bóng trực tiếp summer season? What are regulations on evaluation by scores for continuing education students at lower secondary level in Vietnam? (Image from đá bóng trực tiếp Internet)
What are regulations on evaluation by scores for continuing education students at lower secondary level in Vietnam?
Pursuant to Clause 2, Article 5 ofCircular 43/2021/TT-BGDDT, đá bóng trực tiếp regulations on evaluation by scores for continuing education students at lower secondary level in Vietnam are as follows:
- Teachers use scores to evaluate đá bóng trực tiếp results of students' practice and study.
- đá bóng trực tiếp assessment by scores is utilized in regular evaluations, periodic evaluations through forms of testing, and assessing đá bóng trực tiếp performance of practice and study tasks suitable to đá bóng trực tiếp specific characteristics of đá bóng trực tiếp subject.
What are regulations on evaluation of đá bóng trực tiếp practice result of continuous education students at đá bóng trực tiếp lower secondary level in each semester in Vietnam?
Pursuant to Clause 2, Article 8 ofCircular 43/2021/TT-BGDDT, đá bóng trực tiếp practice results of continuous education students at đá bóng trực tiếp lower secondary level each semester are evaluated according to four levels as follows:
- Good Level: Meets đá bóng trực tiếp required standards of qualities stipulated in đá bóng trực tiếp continuous education curriculum and demonstrates many outstanding traits.
- Fair Level: Meets đá bóng trực tiếp required standards of qualities stipulated in đá bóng trực tiếp continuous education curriculum and shows outstanding traits but has not reached đá bóng trực tiếp Good level.
- Pass Level: Meets đá bóng trực tiếp required standards of qualities stipulated in đá bóng trực tiếp continuous education curriculum.
- Not Pass Level: Does not meet đá bóng trực tiếp required standards of qualities stipulated in đá bóng trực tiếp continuous education curriculum.
