Question

ПОМОГИТЕ ПОЖАЛУЙСТА СДЕЛАТЬ ГЕОГРАФИЮ! 60 БАЛЛОВ! ОПИСАНИЕ СУБТРОПИЧЕСКОГО КЛИМАТИЧЕСКОГО ПОЯСА ЕВРАЗИИ. 1. В КАКОМ КЛИМАТИЧЕСКОМ ПОЯСЕ И В КАКОЙ ОБЛАСТИ РАСПОЛОЖЕНА ТЕРРИТОРИЯ? 2. СРЕДНИЕ ТЕМПЕРАТУРЫ ИЮЛЯ И ЯНВАРЯ. В КАКОМ НАПРАВЛЕНИИ ОНИ ИЗМЕНЯЮТСЯ И ПОЧЕМУ? 3. ГОСПОДСТВУЮЩИЕ ВЕТРЫ. ( ПО СЕЗОНАМ ) 4. ГОДОВОЕ КОЛ-ВО ОСАДКОВ И ИХ РЕЖИМ. ЧЕМ ОБЪЯСНИТЬ РАЗЛИЧИЕ В КОЛИЧЕСТВЕ ОСАДКОВ? ПОМОГИТЕ ПОЖАЛУЙСТА!

Answer 1

1. За полярным кругом
2. -20 и ниже .изменяются с запада на восток , с запада теплее
3. На западе преобладают теплые атлантические ветры
4. Менее 400 мм

Answer 2

Description of the Subtropical Climatic Zone in Eurasia

The subtropical climatic zone in Eurasia is characterized by its location in the southern part of the continent, primarily in the regions around the Mediterranean Sea, the Black Sea, and the Caspian Sea. This climatic zone is known for its warm to hot summers and mild winters, with a distinct pattern of temperature and precipitation changes throughout the year.

1. Location of the Subtropical Climatic Zone in Eurasia

The subtropical climatic zone in Eurasia is primarily located in the southern parts of the continent, including countries such as Spain, Italy, Greece, Turkey, Iran, and parts of Russia. It encompasses regions that are close to or bordering the Mediterranean Sea, the Black Sea, and the Caspian Sea.

2. Average Temperatures in July and January and their Variation

In the subtropical climatic zone of Eurasia, the average temperatures in July are generally high, ranging from 25 to 35 degrees Celsius (77 to 95 degrees Fahrenheit). This is due to the high solar radiation received during the summer months in these regions. The warm temperatures are influenced by the proximity to large bodies of water, which help moderate the climate.

In contrast, the average temperatures in January are relatively mild, ranging from 5 to 15 degrees Celsius (41 to 59 degrees Fahrenheit). The mild winter temperatures are a result of the moderating effect of the surrounding seas, which help retain heat and prevent extreme cold temperatures.

The variation in temperatures between July and January is primarily influenced by the movement of air masses and the position of the subtropical high-pressure systems. During summer, the subtropical high-pressure systems move northward, bringing warm air and high temperatures to the region. In winter, these systems move southward, resulting in milder temperatures.

3. Dominant Winds by Season

The dominant winds in the subtropical climatic zone of Eurasia vary by season. In summer, the prevailing winds are known as the "Mistral" in the Mediterranean region and the "Etesian" in the Black Sea region. These winds blow from the north and northwest, bringing relatively cooler air from higher latitudes.

In winter, the dominant winds change direction. In the Mediterranean region, the winds are known as the "Sirocco" or "Chamsin" and blow from the south or southeast, bringing warm and dry air from the Sahara Desert. In the Black Sea region, the winds are known as the "Bora" and blow from the northeast, bringing cold air from the Eurasian continent.

4. Annual Precipitation Amount and Regime

The annual precipitation amount in the subtropical climatic zone of Eurasia varies depending on the specific location within the zone. Generally, these regions receive moderate to high amounts of rainfall throughout the year, with some variations.

The Mediterranean region, for example, experiences a Mediterranean climate characterized by dry summers and wet winters. The majority of the precipitation occurs during the winter months, while the summer months are relatively dry. This pattern is influenced by the movement of the subtropical high-pressure systems, which bring moist air from the Mediterranean Sea during winter.

In contrast, the Black Sea region has a more evenly distributed rainfall pattern throughout the year. The region receives precipitation from both maritime and continental air masses, resulting in a relatively higher annual precipitation amount compared to the Mediterranean region.

The differences in precipitation amounts within the subtropical climatic zone can be attributed to various factors, including the proximity to large bodies of water, the topography of the region, and the influence of prevailing winds. These factors contribute to the variation in the amount and distribution of rainfall.

Please note that the information provided above is based on general characteristics of the subtropical climatic zone in Eurasia. Specific details may vary depending on the location within the zone.