What are the seasonal differences in precipitation between the north east and south west of Sri Lank

Sri Lanka. The seasonal differences in precipitation in the northeastern and southwestern parts of the island and the reasons for them are influenced by the trade winds and topography. Under the influence of northerly winds, the South Asian winter monsoon brought water vapor with landfall and formed precipitation in eastern Sri Lanka. The western side has a lot of precipitation in summer, because it is affected by the southwest monsoon, which makes landfall and is uplifted by the terrain to form abundant precipitation.

The island of Sri Lanka is pear-shaped, and the south-central part of Sri Lanka is a plateau, of which Mount Piduruta Lagle is 2,524 meters above sea level, which is the highest point in the country. The northern and coastal areas are plains, with the northern coastal plain being wide and the southern and western coastal plains relatively narrow, both at an altitude of 150 meters. in the Indian Ocean.

To the northeast is Bangladesh.

Bay. The central part is a plateau with Adam's Peak. Sri Lanka belongs to the South Asian monsoon region and has a tropical monsoon climate.

The island of Sri Lanka has a total area of 65,610 square kilometers and is located in the south of Asia, with the main body of latitude and longitude.

It is 8 degrees north latitude and 80 degrees east longitude, and is an island country in the Indian Ocean at the southern tip of the South Asian subcontinent, with beautiful scenery, known as "the pearl of the Indian Ocean" and "the country of gems".

and "Lion Country". It is separated from the Indian peninsula by the Strait of Banks to the northwest. Close to the equator, it is like summer all year round, with an average annual temperature of 28. The average annual precipitation ranges from 1283 to 3321 mm.

Sri Lanka has a tropical monsoon climate. It is like summer all year round, and the average annual temperature is 28. The average annual precipitation ranges from 1283 to 3321 mm.

Average maximum temperature, average minimum temperature in coastal areas. Average maximum temperature and average minimum temperature in mountainous areas. There are no four seasons, only the rainy season and the dry season, which are from May to August and November to February, when the southwest and northeast monsoons pass through Sri Lanka.

Annual rainfall ranges from 2540 mm to 5080 mm in the southwest and less than 1250 mm in the northwest and southeast.

Sri Lanka is an island country with a tropical monsoon climate and abundant precipitation. Its precipitation mainly comes from the water vapor brought by the southwest monsoon and northeast winds, so the spatial distribution of annual precipitation is characterized by more precipitation in the southwest and northeast, and less precipitation in the southeast and northwest.

1. You're wrong, right? Why does the southwestern tip of Sri Lanka Island get more precipitation in summer? Why is there more precipitation in the Northeast in winter?

2. Reason: There is a lot of winter precipitation in the east of Sri Lanka, because due to the influence of northerly winds, the South Asian winter monsoon landfalls to bring water vapor, and it makes landfall in the east of Sri Lanka to form precipitation; The western side has a lot of precipitation in summer, because it is affected by the southwest monsoon, which makes landfall and is uplifted by the terrain to form abundant precipitation.

2. Just look at the picture:

Characteristics of precipitation distribution: more precipitation in the west and less in the east.

Reason: The South Island of New Zealand is located in a prevailing westerly wind belt; The western part is located on the windward slope of the humid western windy belt from the ocean, with heavy terrain rain; In the east, the leeward of the westerly wind zone is sloppy and has little precipitation.

Sri Lanka East.

The winter precipitation on the coming side is due to the influence of northerly winds, and the landfall of the South Asian winter monsoon brings water vapor, which makes landfall in the eastern part of Sri Lanka to form precipitation. The western side has a lot of precipitation in summer, because it is affected by the southwest monsoon, which makes landfall and is uplifted by the terrain to form abundant precipitation.

Singapore is located in a tropical rainforest climate zone with abundant precipitation but a severe shortage of water resources. The main reasons are (1) although Singapore has a lot of precipitation, it has a small land area, a lack of large rivers, low runoff, and a serious shortage of water resources; (2) The level of urbanization is high, the ground is hardened in a large area, it is difficult for rainwater to infiltrate, the groundwater cannot be recharged, and the groundwater resources are insufficient; (3) The densely populated production and domestic water consumption is large, and the contradiction between population and water resources is acute.

Characteristics of precipitation distribution in the South Island of New Zealand: precipitation gradually decreases from west to east, that is, the precipitation is more in the west and less in the east.

Reason: New Zealand's South Island is located in a westerly belt; The western part is located on the windward slope of the humid westerly wind belt from the ocean, with terrain and rain; The eastern part is located on the leeward slope of the westerly belt and has little precipitation.

Distribution characteristics: more in the west and less in the east.

Causes: Located in the westerly wind belt, westerly winds blow all year round, bringing a lot of water vapor The west is located on the windward slope, and it rains terrain; The eastern part is located on the leeward slope and is a rain shadow area with little precipitation.

Geographical type of agriculture: dairy and livestock.

Conditions: Temperate oceanic climate with uniform precipitation and abundant aquatic vegetation. Located in the southwest of the Pacific Ocean, the transportation is convenient, the science and technology are developed, and the processing and insulation technology is good.

Ceylon is an island region, the northern mountains, the presence of the Indian Peninsula and the influence of the earth's rotation affect the deflection of the Mongolian winter monsoon to the south, the northeast monsoon is characterized by dry and little rain during the period of passing through the region, so Sri Lanka has more rain in summer, and the temperature is uniform throughout the year, which does not belong to the tropical rainforest climate.

The northern part of the island of Sri Lanka is a mountain range, the existence of the Indian Peninsula and the influence of the earth's rotation The Mongolian winter monsoon deflects into the northeast monsoon when it moves southward, and the northeast monsoon is characterized by dry and little rain during the period after the region, so Sri Lanka only has more rain in summer, and the temperature is uniform throughout the year, so it is not all tropical rainforest climate, thank you!

Climatic reasons: dry, hot, much like Africa.