Climate of Vietnam
Vietnam's climate, because its in the tropics and strongly influenced by the South China Sea, has a monsoon-influenced tropical climate typical of that of mainland Southeast Asia. In the north, the climate is monsoonal with four distinct seasons while in the south, the climate is tropical monsoon with two seasons. In addition temperate climate exists in mountainous areas, which are found in Sa Pa, Da Lat while a more continental climate exists in Lai Chau Province and Son La Province.
The diverse topography, wide range of latitudes, and influences from the South China Sea lead to climatic conditions varying significantly between regions. 20% of Vietnam's total surface area is low-elevation coastal area making the country highly vulnerable to climate change effects and the rising sea levels in particular.
Atmospheric circulation
The atmospheric circulation influencing Vietnam is part of the Southeast Asian monsoon circulation that is characterized by 3 distinct features:- In addition to being influenced by the South Asian monsoon in summer, parts of Vietnam are strongly influenced by the Northeast Asian monsoon, particularly during winter.
- In addition to being influenced by tropical, subtropical and temperate circulations from the Northern Hemisphere, the atmospheric circulation influencing Vietnam are closely associated with subtropical and tropical circulations from the Southern Hemisphere.
- Vietnam's climate is strongly influenced by its location to the adjacent sea in all seasons.
Seasons
During winter, polar air originating from the Siberian High penetrate deeply into the low latitudes, facilitated by the eastern Tibetan Plateau that funnels the air southwards in a northeast direction. Many cold fronts can penetrate into Vietnam during winter of which there are 3-4 occurrences every month in northern Vietnam. This leads to cold temperatures where temperatures drop by. Cold weather, occasionally extreme cold can persist for a long time, being characterized by a long stretch of cloudless or partly cloudy days in the first half of winter or a long stretch of cloudy and drizzly conditions in the latter half of winter. Cold weather occurs more frequently in the north than in the south due to cold fronts penetrate the north more frequently.In summer, the general wind pattern are southwesterly winds in the southern parts of Vietnam and southeasterly winds in northern Vietnam. The predominantly air blocks in Vietnam are the equatorial and tropical blocks that originate from high pressure systems in the Southern Hemisphere, and a maritime tropical block originating from the subtropical high pressure system in the Pacific Ocean. In addition, during summer, Vietnam is influenced by tropical air from the Bay of Bengal which occurs when a continental low pressure originating from South Asia moves eastwards towards Vietnam, covering almost all of Vietnam and southern China; this causes hot, dry weather in the North Central Coast as westerly winds descend and warm adiabatically on the eastern slopes of the Annamite Range. On average, 11 storms and tropical low pressures develop in the South China sea during summer of which half are tropical cyclones that originate from the western Pacific. These storms and cyclones then move westwards towards Vietnam. On average, Vietnam is affected by 6–8 typhoons or tropical cyclones per year.
Spring and Fall are transitional seasons. The atmospheric circulation in these seasons represent a transition between winter–summer and summer–winter respectively.
In general, the northern parts of the country have four seasons: winter, spring, summer, and fall. In the south, only two seasons are present: a dry and a wet season.
Temperature
Mean annual temperatures in the country, based on meteorological data from weather stations range from in Hoang Lien Son to. At the highest altitudes in the Hoang Lien Son range, mean annual temperatures is only. As temperatures vary by altitude, temperatures decrease by for every increase in altitude. The lowest mean annual temperatures are found in the mountainous areas where the altitude is higher and in northern areas due to their higher latitudes. Because Vietnam is strongly influenced by the monsoon, the mean temperatures in Vietnam are lower than other countries located at the same latitude in Asia.In winter, mean temperatures range, decreasing from south to north, and by increases in altitude. In the coolest month, mean temperatures range from in the northern highlands to in the southern highlands. Generally, mean winter temperatures are below in many northern locations. In addition to lower insolation in winter, the Northeast Monsoon contributes to colder conditions. Many mountainous areas in the north have experienced subzero conditions. In contrast, temperatures in the Spratly Islands never falls below. In summer, mean temperatures vary between. The highest temperatures normally occurs in March–May in the south and May–July in the north. This is due to the fact that in the north, drizzle predominates leading to a slight temperature increases in February and March before increasing from April–August while in the south, the temperature increase is much larger. Consequentially, the south reaches their highest temperatures in late winter while in the north, they occur in July and August due to this. Temperatures in summer are relatively equal among the northern and southern parts of the country with differences being mostly due to altitude.
Precipitation
Mean annual rainfall in the country ranges from although most places in Vietnam receive between. The majority of rainfall occurs during the rainy season, which is responsible for 80%–90% of the annual precipitation. Generally, northern parts of the country receive more rainfall than southern parts of the country. Islands located in the north general receive less rainfall than the adjacent mainland while in the south, this is reversed where islands such as Phu Qouc receive more rainfall than the adjacent mainland. The annual average number of rainy days ranges from 60–200 in which most days have rainfall averaging less than. The amount of rainy days in a month usually corresponds with the mean monthly precipitation although in the north and north central coast, drizzle is common in winter, leading to higher amounts of rain days. For example, there are more rainy days in the drier season during winter in Yen Bai Province due to drizzle than there are rainy days in the main rainy season. Drizzle is a weather phenomenon that is characteristic of the weather in winter in the north and north central coast. Days with thunderstorms occur 20–80 days per year, which are more common in the south and north, and more common in mountainous areas than coastal delta. Thunderstorms can occur year-round although they are the most common during the rainy season. In the highest peaks in the north in Sa Pa, Tam Dao, and Hoang Lien Son, snowfall can occur.Depending on the region, the onset of the rainy season differs: In the North West and North East, the rainy season beings in April–May with a peak in July–August and ends in September and October. In the Red River Delta, the rainy season beings in April–May with a peak in July–August and ends in October and November. On the North Central Coast, the rainy season begins in August and September, reaching a peak in October and November before ending in November and December. For the South Central Coast, the rainy season begins in August and September, reaching a peak in October and November before ending in December. In the Central Highlands, the rainy season begins in April and May that peaks in August before ending in October and November. Finally, the South has its rainy season beginning in May that peaks in September before ending in November.
Regional climate
Based on geographic and climatic conditions, there are 7 different climatic regions in Vietnam: Northwest, Northeast, North Delta, North Central, South Central, Central Highlands, and the South. Generally, these 7 different climatic regions are grouped into 2 main types: The North, North Central ) which includes all areas north of the Hải Vân Pass and the South which includes all areas south of the Hải Vân Pass. These climatic regions are based on time of rainy season and other climatic elements such as insolation, sunshine, temperature, precipitation, and humidity. The diverse topography, wide range of latitudes, and influences from the South China Sea lead to climatic conditions varying significantly between regions.Northwest
The Northwest region includes the provinces of Lai Châu, Sơn La, and Điện Biên. The climate is characterized by cold, dry, sunny winters in which hoarfrost is common in many years. Summers are hot and rainy, coinciding with the rainy season although there is a high frequency of hot, dry days caused by westerly winds. Valleys are sheltered from wind, leading to a longer dry season and lower annual rainfall. The dry season usually lasts for 4–5 months. The average annual amount of sunshine hours is 1,800 to 2,000. Owing to diverse terrain and climate in this region, this leads to different types of forests being present.Northeast
The Northeast region includes the northern and northeastern provinces: Lao Cai, Yen Bai, Hoa Binh, Ha Giang, Tuyen Quang, Phu Tho, Cao Bang, Lang Son, Bac Kan, Thai Nguyen, and Quang Ninh. The climate is strongly influenced by the northeast monsoon. Winters are cold, cloudy that is characterized by drizzle. The cold comes earlier than other provinces. Summers are hot and rainy that coincide with the rainy season. However, unlike the northwest, dry conditions are rare due to a low frequency of westerly winds. The rainy season usually lasts from May–September although its duration can vary from 4 to 10 months. In the Hoang Lien Son mountains, winters are cold where snowfall and hoarfrost can occasionally occur. These mountains have the highest rainfall in the country. The average annual amount of sunshine hours is 1,400 to 1,700.Mean annual temperatures in the coastal areas are around in which the coldest month has a mean temperature of and the hottest month has a mean temperature of. Average annual rainfall in coastal areas is approximately.
North Delta (Red River Delta)
The North Delta includes the provinces of Phu Tho, Vinh Phuc, Bac Giang, Bac Ninh, Hanoi, Hai Phong, Hai Duong, Hung Yen, Ha Nam, Nam Dinh, Thai Binh, and Ninh Binh. Winters are characterized as being cold with large amounts of drizzle and few sunshine while summers are hot, rainy with few dry days. Hot, dry conditions caused by westerly winds during summer are rare. The region has a positive water balance for 10 months of the year. The average annual amount of sunshine hours is 1,400 to 1,700.Mean annual temperatures in the coastal areas are around in which the coldest month has a mean temperature of and the hottest month has a mean temperature of. Average annual rainfall in coastal areas is approximately.
North Central (North Central Coast)
The North Central Coast includes the provinces of Thanh Hoa, Nghe An, Ha Tinh, Quang Binh, Quang Tri, and Thừa Thiên-Huế. Winters are characterized by cold, cloudy weather with frequent drizzle, being under the influence of the northeast monsoon. Summers are characterized by hot, dry weather owing to westerly winds. The region averages between 1,500 and 1,700 hours of sunshine per year.Mean annual temperatures are around in which the coldest month has a mean temperature of and the hottest month has a mean temperature of. Average annual rainfall in coastal areas is approximately. The rainy season occurs in the last 6 months of the year with September and October having the highest rainfall.
South Central (South Central Coast)
, Quang Nam, Quang Ngai, Binh Dinh, Phu Yen, Khanh Hoa, Ninh Thuan, and Binh Thuan are the provinces that are part of the South Central Coast region. Winters are warm and sunny while summers are hot and dry owing to a high frequency of the westerly winds. The average annual amount of sunshine hours is 2,000 to 2,500.Mean annual temperatures are around in which the coldest month has a mean temperature of and the hottest month has a mean temperature of. In contrast to the North Central Coast, the temperature difference between the coldest and hottest months is much smaller. Average annual rainfall in coastal areas is approximately although some areas in the southern parts of the region receive between. As one progresses southward, the rainy season shifts away from the end of year and vice versa. In general, the rain season starts in September and ends in December or January. Northern parts of the region receive more rainfall than in the southern parts of the region.
Central Highlands
The Central Highlands includes Kon Tum Province, Gia Lai Province, Dak Lak Province, Dak Nong Province, and Lam Dong Province. Owing to the higher altitude, temperatures are lower than other regions at comparable latitudes. Winters are dry while summers are characterized by high rainfall. The average annual amount of sunshine hours is 2,000 to 2,500.The average annual temperature is. During winter, mean temperatures can fall below. The coldest month is January where minimum temperatures can occasionally fall below. The highest temperatures occur in late winter and early summer. This is usually during March and April.
The South
The South corresponds to the Southeast region, and the Mekong Delta region. It also includes some parts of Binh Thuan Province. The climate of the south is strongly influenced by the southwest monsoon. The climate of this region is characterized by high temperatures year round and sunny weather. Mean annual temperatures in coastal areas are around that is fairly even throughout the year with little difference between the coldest and hottest months of the year. Average annual rainfall in coastal areas is approximately in which the rainy season is between May to November. The average annual sunshine hours ranges from 2,400 to 3,000. Sunshine hours are higher in the northeastern parts of the region where they exceed over 2,700 hours per year while in the west, it is around 2,300 hours per year.Extremes
The highest temperature ever recorded in Vietnam was, which was recorded in Huong Khe District, Ha Tinh Province on 20 April 2019.The coldest temperature recorded in Vietnam was in Sa Pa on 4 January 1974. A record low of was also record in Hoang Lien on 1 January 1974 and 6 January 1974. For ground temperatures, the lowest ground temperature ever record was in Sa Pa in 31 December 1975 while the highest was in Buôn Ma Thuột in 23 May 1982. Absolute record low ground temperatures tend to be lower than record low air temperatures but absolute record high ground temperatures tend to be over higher than the air temperature.
The highest air pressure ever recorded in Vietnam was at the Lang weather station on 18 November 1996 when a reading of was recorded. The lowest air pressure ever recorded was at Sa Pa on 24 July 1971 with a reading of.
The highest wind recorded in Vietnam was in Quy Nhon in September 1972 although wind velocities over have been recorded in the North Delta, and coastal areas of Quang Ninh Province