Geography of Thailand
Template:Short description Template:Country geography

Thailand is a sovereign state located in the center of Mainland Southeast Asia. The country extends from the southeastern foothills of the Himalayas to the Mekong river, further south to the Gulf of Thailand, and roughly to the middle of the Malay Peninsula and the Andaman Sea of the Indian Ocean. It has a total size of Template:Convert which is the 50th largest in the world.<ref name="cia1">Template:Cite web</ref><ref name=":5">Template:Cite web</ref> The land area lies between latitudes 5° 37' South and 20° 27' North, and between the longitude 97° 22' West and 105° 37' East.<ref name=":5" />
Thailand shares a Template:Convert long international land boundary with Myanmar, Laos, Cambodia and Malaysia. The nation's axial position influenced many aspects of Thailand's society and culture.<ref name=":08">Template:Cite book</ref> Southern Thailand is the only land route from mainland Asia to Malaysia and Singapore. It has an exclusive economic zone of Template:Convert.<ref name=":12" />
Composition and geography
Location
A fertile floodplain and tropical monsoon climate, ideally suited to wet-rice (tham na) cultivation, attracted settlers to this central area in preference to the marginal uplands and the highlands of the northern region or the Khorat Plateau to the northeast.<ref name=":08" />
By the 11th century AD, a number of loosely connected rice-growing and trading states flourished in the upper Chao Phraya Valley.<ref name=":08" /> They broke free from domination of the Khmer Empire, but from the middle of the 14th century gradually came under the control of the Ayutthaya Kingdom at the southern extremity of the floodplain.<ref name=":08" />
Successive capitals, built at various points along the river, became centers of great Thai kingdoms based on rice cultivation and international commerce.<ref name=":08" /> Unlike the neighboring Khmer and Burmese, the Thai continued to look outward across the Gulf of Thailand and the Andaman Sea toward foreign ports of trade.<ref name=":08" />
European colonisation of Southeast Asia brought a new phase of Southeast Asian commerce in the late-1800s. Thailand (then called Siam) was able to maintain its independence as a buffer zone between British-controlled Burma to the west, British Malaya to the south, and French Indochina to the east.<ref name=":08" /> However, Thailand lost over 50% of its former territory to the expanding claims of French Indochina until 1907. Its central location made the Kingdom of Thailand's position a regional hub that has greatly influenced its society, culture and history. Southern Thailand has a long, narrow shape. It is the only land connection to Malaysia and Singapore.
Mountains
The mountain ranges that run parallel from north to south across Mainland Southeast Asia are one of Thailand's most distinctive geographical features.<ref name="コトバンク1557462" /> The country's highest peak is Doi Inthanon, with an elevation of 2,565 meters.<ref name="Doi Inthanon" /> Major mountain ranges include the Thanon Thong Chai Range, the Daen Lao Range on Thailand's northern edge, and the Tenasserim Range on the border with Myanmar. The average elevation decreases as one moves south.Template:Sfn There are no volcanoes.<ref>No.530 海を漂う軽石 富山市科学博物館、2022年4月1日。2023年10月15日閲覧。</ref> There are 10 mountains over Template:Convert. 148 mountains exceed Template:Convert.
Northern Thailand's mountainous regions like Chiang Mai and Doi Inthanon have chilly air and misty mornings.<ref name=":7">Template:Cite web</ref> However, at high altitudes it does not get colder than 5 °C to 10 °C due to the tropical climate.<ref name=":7" /> There is no snow and frost is rare in the coldest months.<ref name=":7" /> In 1955, snow-like frost was reported in Doi Inthanon.<ref name=":7" />
The 10 tallest mountains in Thailand are located in Northern Thailand. The highest peaks in each part of Thailand are:
| Rank | Name | Thai name | Range | Province | Elevation
(m) |
Observations |
|---|---|---|---|---|---|---|
| 1 | Doi Inthanon | Template:Lang | Thanon Thong Chai | Chiang Mai | Template:Convert | <ref name="Doi Inthanon">Doi Inthanon National Park Template:Webarchive</ref> Highest point in Thailand. Formerly known as Doi Luang |
| 2 | Doi Pha Hom Pok | Template:Lang | Daen Lao | Chiang Mai | 2,285 | <ref>Doi Fahhompok National Park Template:Webarchive</ref> Donner: 2,296 m; highest peak of the Daen Lao Range on the Thai side of the border |
| 3 | Doi Chiang Dao | Template:Lang | Daen Lao | Chiang Mai | 2,175 | <ref name="Donner">Template:Cite book</ref>Template:RP Also known as Doi Luang Chiang Dao. 2,225 m in some sources |
| 4 | Khao Kacheu La | Template:Lang | Tak | 2,152 | <ref name="gmgroup.in.th">GMCAR VOL.13 NO. 185 December 2008 Template:In lang</ref> | |
| 5 | Phu Soi Dao | Template:Lang | Luang Prabang Range | Uttaradit | 2,120 | <ref>Template:Cite web</ref> Highest point of the Luang Prabang Range in Thailand |
| 6 | Phu Khe | Template:Lang | Luang Prabang | Nan | 2,079 | <ref>Template:Cite web</ref><ref>Template:Cite web</ref> |
| 7 | Phu Lo | Template:Lang | Luang Prabang | Nan | 2,077 | <ref name="gmgroup.in.th" /> Also known as Doi Lo<ref>Template:Cite web</ref> |
| 8 | Doi Mae Tho | Template:Lang | Khun Tan | Chiang Rai | 2,031 | <ref name="Khun Chae">Template:Cite web</ref> Highest point of the Khun Tan Range; also known as Doi Lang Ka or Doi Langka Luang |
| 9 | Doi Mae Ya | Template:Lang | Mae Hong Son | 2,005 | <ref>Thai travelTemplate:Dead link</ref> | |
| 10 | Doi Phong Sa Yan | Template:Lang | Mae Hong Son | 2,004 | <ref name="gmgroup.in.th" /> |
Shape

The geographic shape of Thailand resembles an elephant's head with a long trunk.<ref name=":22">Template:Cite web</ref><ref name=":4">Template:Cite web</ref> There are 2 big ears, the Bay of Bangkok is a mouth and Southern Thailand is a long trunk that reaches down the Malay Peninsula.<ref name=":4" /> The westside is the front of the head. The elephant holds deep cultural significance and it's a national symbol of Thailand.<ref name=":22" /><ref name="Thai_Government2">Template:Cite journal</ref> The elephant also symbolizes Thailand’s natural heritage and fills a vital role in the ecosystems of the region.<ref name=":8" />
Plains
Thailand has large plains, valleys and basins.
Forests
The forest cover rate was 63% in the 1940s, but declined to 53.3% in the 1960s and 26.6% in 1991.Template:Sfn It had been declining due to timber exports, urbanization, and development.Template:Sfn Since the late 1980s, the decline has been halted since protective measures such as banning logging of natural forests were implemented.Template:Sfn As of 2020, the Royal Forest Department has classified the country's forests as 31.6% and 38.9% according to the FAO, remaining stable.Template:SfnTemplate:Efn
The Royal Forest Department classifies the country's forests into six categories: mangrove/coastal forest, evergreen forest, evergreen forest, mixed deciduous forest, deciduous dipterocarp forest, and savanna.Template:Sfn Exotic plantations such as eucalyptus and rubber are classified as agricultural land.Template:Sfn Of these, mangrove forests and coastal forests are more prevalent in the south and east, mixed deciduous forests in the north, and deciduous dipterocarp forests and savannas in the northeast.Template:Sfn
Rivers
The main rivers are the Chao Phraya River and the Mekong,<ref name="Britannica" /> as well as the Salween River, Mae Klong, Mun River, Chi River, Tha Chin River, and Bang Pakong River.<ref>Knowledge - Basin Informationタイ水資源局、2023年10月22日閲覧。</ref> Southern Thailand has short and steep rivers due to the narrow peninsula.Template:Sfn The Mekong is partially a natural border between Thailand and Laos for 920 km. It flows from the Golden Triangle in Northern Thailand to Khong Chiam district in Northeastern Thailand.
These are the 10 longest rivers of Thailand:
Lakes
There are around 8000 natural lakes and swamps.<ref name=":6" /> This includes a few large lakes and thousands of small lakes. Songkhla lake is the largest natural lake at Template:Convert.
These are the 9 largest lakes of Thailand:
Islands
Template:See also There are approximately 1,430 islands.<ref>Incredible Islands in Thailand ザ・タイムズ・オブ・インディア、2023年3月9日。2023年10月22日閲覧。</ref> They are relatively small-sized islands and uninhabited islets. Many islands are protected areas in national parks or wildlife sanctuaries. Most islands are near the coasts of Southern Thailand and Eastern Thailand. The largest island is Phuket Template:Convert in the Andaman Sea.<ref name="TAT">Template:Cite web</ref>
These are the 10 largest islands of Thailand:<ref>Template:Cite web</ref>
| Rank | Island name | Thai name | Area
(km2) |
Area
(sq mi) |
Island group |
|---|---|---|---|---|---|
| 1 | Phuket | ภูเก็ต | 543 | 209.65 | |
| 2 | Ko Samui | เกาะสมุย | 229 | 88 | |
| 3 | Ko Chang | เกาะช้าง | 211 | 81 | |
| 4 | Ko Tarutao | เกาะตะรุเตา | 152 | 58.68 | |
| 5 | Ko Pha-ngan | เกาะพะงัน | 125 | 48 | |
| 6 | Ko Kut | เกาะกูด | 105 | 40 | |
| 7 | Ko Yao Yai | เกาะยาวใหญ่ | 92 | 35.5 | |
| 8 | Ko Phra Thong | เกาะพระทอง | 88 | 33.97 | |
| 9 | Ko Lanta Yai | เกาะลันตาใหญ่ | 81 | 31 | |
| 10 | Ko Yao Noi | เกาะยาว | 36 | 13.89 |
Geology
Present-day Thailand is theorized to have formed during the Triassic period when two continental fragments: Shan-Thai and Cimmeria formed during the breakup of Gondwana.Template:Sfn Shan-Thai and Cimmeria collided and merged, eventually moving northward and connecting with Laurasia.Template:Sfn Geologically, Thailand is divided into the Western Zone, which belongs to the Shan-Thai terrane; the Northeastern Zone, which belongs to the Indochina Block; and the Central Zone, which is located between the Western and Northeastern Zones.Template:Sfn
The northeastern part of Thailand is a relatively stable plateau, with only the Mesozoic, Jurassic and Cretaceous sandstone and shale being uplifted by Tertiary tectonic activity.[30] Most of the rest of the country exhibits a complex geological structure, consisting primarily of Paleozoic limestone and other sedimentary rocks, and Precambrian metamorphic rocks.Template:Sfn Late Mesozoic granite is found in the Western Zone, while Paleozoic and Mesozoic neutral or acidic volcanic rocks are abundant in the Central Zone.Template:Sfn
Although seismic activity is not particularly high, there are 13 known active faults, mainly in the northwest and central-southwest, and in 2014 the northern part of the country experienced one of the largest earthquakes ever recorded (the 2014 Mae Lao earthquake), measuring 6.3 on the Richter scale.<ref>Template:Cite report</ref>
General soil conditions
| Type | Description | Map |
|---|---|---|
| Soils of the alluvial plains and the lower terraces |
|
|
| Soils of the higher terraces and the low plateaus |
| |
| Soils of the Hills and the mountains |
|
Main land forms
Soils and surface rocks
Topography and drainage

The most conspicuous features of Thailand's terrain are high mountains, a central plain, and an upland plateau.<ref name=":08" /> Mountains cover much of northern Thailand and extend along the Myanmar border down through the Kra Isthmus and the Malay Peninsula.<ref name=":08" /> The central plain is a lowland area drained by the Chao Phraya River and its tributaries, the country's principal river system, which feeds into the delta at the head of the Bay of Bangkok.<ref name=":08" /> The Chao Phraya system drains about one-third of the nation's territory.<ref name=":08" /> In the northeastern part of the country the Khorat Plateau, a region of gently rolling low hills and shallow lakes, drains into the Mekong River via the Mun River.<ref name=":08" /> The Mekong system empties into the South China Sea and includes a series of canals and dams.<ref name=":08" />
Together, the Chao Phraya and Mekong systems sustain Thailand's agricultural economy by supporting wet-rice cultivation and providing waterways for the transport of goods and people.<ref name=":08" /> In contrast, the distinguishing natural features of peninsular Thailand are long coastlines, offshore islands, and mangrove swamps.<ref name=":08" /> A recent global remote sensing analysis suggested that there were Template:Convert of tidal flats in Thailand, making it the 45th ranked country in terms of tidal flat extent.<ref>Template:Cite journal</ref>
Area
Thailand is the 50th largest country in the world and the 3rd largest country in Southeast Asia after Indonesia and Myanmar.<ref name=":3">Template:Cite web</ref>
| Total | Land | Water | Comparative area |
|---|---|---|---|
|
|
|
|
Boundaries
| Land boundaries | Coastline | Water |
|---|---|---|
|
|
|
Maritime claims
| Territorial sea | Exclusive economic zone | Continental shelf |
|---|---|---|
|
|
Extreme points
Extreme elevations
| Heading | Location | Province | Bordering entity | Coordinates | Ref |
|---|---|---|---|---|---|
| North | Mae Sai District | Chiang Rai Province | Myanmar | Template:Coord | |
| South | Betong District | Yala Province | Malaysia | Template:Coord | |
| East | Khong Chiam District | Ubon Ratchathani Province | Laos | Template:Coord | |
| West | Mae Sariang District | Mae Hong Son Province | Myanmar | Template:Coord |
Extreme altitudes
| Extremity | Name | Thai name | Altitude | Province | Coordinates | Ref |
|---|---|---|---|---|---|---|
| Highest | Doi Inthanon | ดอยอินทนนท์ | Template:Convert | Chiang Mai Province | Template:Coord | |
| Lowest
(man-made) |
Boh Yai mine<ref name="bohyai">Template:Cite web</ref> | เหมืองบ่อยาย | Template:Convert<ref name="bohyai"/> | Kanchanaburi Province | Abandoned mine, closed in 1997. Surveyed up to -106 m.<ref name="bohyai"/> | |
| Lowest
(natural) |
Gulf of Thailand | อ่าวไทย | Template:Convert | Surrounding provinces |
Regions & provinces

Thailand is a unitary state; the administrative services of the executive branch are divided into three levels by the Law on the Organization of National Government, BE 2534 (1991): central, provincial and local. Thailand's regions are divided into a total of 76 provinces (จังหวัด , changwat) plus Bangkok, which is a special administrative area. These are first-level administrative divisions.
The National Research Council divides Thailand into six geographical regions, based on natural features including landforms and drainage, as well as human cultural patterns.<ref>Template:Cite web</ref> They are:
- North
- Northeast
- Central
- East
- West
- South<ref>Mundus. Wissenschaftliche Verlagsgesellschaft. 1981. p. 65. Retrieved 17 January 2012.</ref>
Although Bangkok geographically is part of the central plain, as the capital and largest city this metropolitan area may be considered in other respects a separate region.<ref name=":08" />
Each of the six geographical regions differs from the others in population, basic resources, natural features, and level of social and economic development.<ref name=":08" /> The diversity of the regions is in fact the most pronounced attribute of Thailand's physical setting.<ref name=":08" />
| Name | Thai name | Area total | Provinces | Description | Image |
|---|---|---|---|---|---|
| Northern Thailand | ภาคเหนือ | 96,077 km2<ref name="RFD">Template:Cite web</ref> | Northern Thailand is a mountainous area. Parallel mountain ranges extend from the Daen Lao Range (ทิวเขาแดนลาว), in the southern region of the Shan Hills, in a north-south direction, the Dawna Range (ทิวเขาดอยมอนกุจู) forming the western border of Thailand between Mae Hong Son and the Salween River,<ref>Northern Thailand Template:Webarchive</ref> the Thanon Thong Chai Range (เทือกเขาถนนธงชัย), the Khun Tan Range (ดอยขุนตาน), the Phi Pan Nam Range (ทิวเขาผีปันน้ำ), as well as the western part of the Luang Prabang Range (ทิวเขาหลวงพระบาง).<ref>ดร.กระมล ทองธรรมชาติ และคณะ, สังคมศึกษา ศาสนาและวัฒนธรรม ม.1, สำนักพิมพ์ อักษรเจริญทัศน์ อจท. จำกัด, 2548, หน้า 24-25</ref>
These high mountains are incised by steep river valleys and upland areas that border the central plain.<ref name=":08" /> Most rivers, including the Nan, Ping, Wang, and Yom, unite in the lowlands of the lower-north region and the upper-central region. The Ping River and the Nan River unite to form the Chao Phraya River. The northeastern part is drained by rivers flowing into the Mekong basin, like the Kok and Ing. The Thi Lo Su Waterfall in Tak province is claimed to be the tallest and highest waterfall in Thailand. Traditionally, these natural features made possible several different types of agriculture, including wet-rice farming in the valleys and shifting cultivation in the uplands.<ref name=":08" /> The forested mountains also promoted a spirit of regional independence.<ref name=":08" /> Forests, including stands of teak and other economically useful hardwoods that once dominated the north and parts of the northeast, had diminished by the 1980s to 130,000 km2.<ref name=":08" /> In 1961 they covered 56% of the country, but by the mid-1980s forestland had been reduced to less than 30% of Thailand's total area.<ref name=":08" /> |
||
| Northeastern Thailand | ภาคตะวันออกเฉียงเหนือ | 167,718 km2<ref name="TDD">Template:Cite web</ref> | The northeast (aka Isan), with its poor soils, is not favoured agriculturally.<ref name=":08" /> However, sticky rice, the staple food of the region, which requires flooded, poorly drained paddy fields, thrives and where fields can be flooded from nearby streams, rivers and ponds, often two harvests are possible each year. Cash crops such as sugar cane and manioc are cultivated on a vast scale, and to a lesser extent, rubber. Silk production is an important cottage industry and contributes significantly to the economy.
The region consists mainly of the dry Khorat Plateau which in some parts is extremely flat, and a few low but rugged and rocky hills, the Phu Phan Mountains.<ref name=":08" /> The short monsoon season brings heavy flooding in the river valleys.<ref name=":08" /> Unlike the more fertile areas of Thailand, the northeast has a long dry season, and much of the land is covered by sparse grasses.<ref name=":08" /> Mountains ring the plateau on the west and the south, and the Mekong delineates much of the northern and eastern rim.<ref name=":08" /> Some varieties of traditional medicinal herbs, particularly of the Genus Curcuma, family Zingiberaceae, are indigenous to the region. |
||
| Central Thailand | ภาคกลาง | 91,798.64 km2 | The "heartland", central Thailand, is a natural self-contained basin often termed "the rice bowl of Asia".<ref name=":08" /> The complex irrigation system developed for wet-rice agriculture in this region provided the necessary economic support to sustain the development of the Thai state from the 13th century Sukhothai Kingdom to contemporary Bangkok.<ref name=":08" />
Here the rather flat unchanging landscape facilitated inland water and road transport.<ref name=":08" /> The fertile area was able to sustain a dense population, 422 people per square kilometre in 1987, compared with an average of 98 for the country as a whole.<ref name=":08" /> The terrain of the region is dominated by the Chao Phraya and its tributaries and by the cultivated paddy fields.<ref name=":08" /> Metropolitan Bangkok, the focal point of trade, transport, and industrial activity, is on the southern edge of the region at the head of the Gulf of Thailand and includes part of the Chao Phraya delta.<ref name=":08" /> |
||
| Eastern Thailand | ภาคตะวันออก | 34,481 km2 | Eastern Thailand lies between the Sankamphaeng Range, which forms the border of the northeastern plateau to the north, and the Gulf of Thailand to the south. The western end of the Cardamom Mountains, known in Thailand as Thio Khao Banthat, extends into eastern Thailand. The geography of the region is characterised by short mountain ranges alternating with small basins of short rivers which drain into the Gulf of Thailand.
Fruit is a major component of agriculture in the area, and tourism plays a strong part in the economy. The region's coastal location has helped promote the Eastern Seaboard industrial development, a major factor in the economy of the region. |
||
| Western Thailand | ภาคตะวันตก | 53,769 km2 | Thailand's long mountainous border with Myanmar continues south from the north into western Thailand with the Tenasserim Hills, known in Thailand as Thio Khao Tanaosi (เทือกเขาตะนาวศรี). The geography of the western region of Thailand, like the north, is characterised by high mountains and steep river valleys.
Western Thailand hosts much of Thailand's less-disturbed forest areas. Water and minerals are also important natural resources. The region is home to many of the country's major dams, and mining is an important industry in the area. |
||
| Southern Thailand | ภาคใต้ | 73,848 km2 | Southern Thailand, part of a narrow peninsula, is distinctive in climate, terrain, and resources.<ref name=":08" /> Its economy is based on tourism, and palm oil and rubber plantations.Template:Citation needed In Krabi Province, for example, palm plantations occupy 980,000 rai (1,568 km2), or 52% of the province's farmland.<ref>Template:Cite news</ref> Other sources of income include coconut plantations, tin mining.<ref name=":08" />
Rolling and mountainous terrain and the absence of large rivers are conspicuous features of the south.<ref name=":08" /> North-south mountain barriers and impenetrable tropical forest caused the early isolation and separate political development of this region.<ref name=":08" /> The Songkhla Lake is the largest natural lake in Thailand. International access through the Andaman Sea and the Gulf of Thailand made the south a crossroads for both Theravada Buddhism, centered at Nakhon Si Thammarat, and Islam, especially in the former Pattani Kingdom on the border with Malaysia.<ref name=":08" /> |
Climate



Thailand's climate is influenced by seasonal monsoon winds (the southwest and northeast monsoons).<ref name="tmd">Template:Cite web</ref>Template:Rp
Most of Thailand has a "tropical wet and dry or savanna climate" type (Köppen's Tropical savanna climate).<ref>Template:Cite web</ref> The majority of the south as well as the extreme east have a tropical monsoon climate. Parts of the south also have a tropical rainforest climate.
Seasons
Thailand has three seasons: summer, rainy, and winter.<ref name=":2">Template:Cite web</ref><ref name="tmd" />Template:Rp
| Season name<ref name=":2" /> | Thai name | Month | Description |
|---|---|---|---|
| Summer | ฤดูร้อน | Mid-February until mid-May | The summer season (aka pre–monsoon) runs from mid-February until mid-May and brings warmer weather.<ref name=":2" /><ref name="tmd" />Template:Rp |
| Rainy | ฤดูฝน | mid-May to mid-October | The rainy season (aka southwest monsoon) is mid-May to mid-October and prevails over most of the country.<ref name=":2" /><ref name="tmd" />Template:Rp Moist air moves from the Indian Ocean to Thailand, causing abundant rain over most of the country.<ref name="tmd" /> August and September are the wettest period of the year.<ref name="tmd" />Template:Rp This can occasionally lead to floods.<ref name="tmd" />Template:Rp In addition to rainfall caused by the southwest monsoon, the Intertropical Convergence Zone (ITCZ) and tropical cyclones also contribute to producing heavy rainfall during the rainy season.<ref name="tmd" /> Dry spells commonly occur for one to two weeks from June to early-July.<ref name="tmd" />Template:Rp This is due to the northward movement of the ITCZ to southern China.<ref name="tmd" />Template:Rp |
| Winter | ฤดูหนาว | mid-October to Mid-February | The winter season (aka northeast monsoon) is active from mid-October till mid-February.<ref name=":2" /><ref name="tmd" /> It brings cold and dry air from China over most of Thailand.<ref name="tmd" />Template:Rp In southern Thailand, the northeast monsoon brings mild weather and abundant rainfall on the eastern coast of that region.<ref name="tmd" />Template:Rp However most of Thailand experiences dry weather and mild temperatures during this season.<ref name="tmd" />Template:RpTemplate:Rp An exception is the southern part of Thailand which receives abundant rainfall, particularly during October to November.<ref name="tmd" />Template:Rp |
Due to their inland location and latitude, the north, northeast, central, and eastern parts of Thailand experience a long period of warm weather.<ref name=tmd/>Template:Rp During the hottest time of the year (March to May), temperatures usually reach up to Template:Convert or more, with the exception of coastal areas where sea breezes moderate afternoon temperatures.<ref name=tmd/>Template:Rp In contrast, outbreaks of cold air from China can bring colder temperatures; in some areas (particularly the north and northeast) close to or below Template:Convert.<ref name=tmd/>Template:Rp Southern Thailand has mild weather year-round, with less diurnal and seasonal variations in temperatures, due to maritime influences.<ref name=tmd/>Template:Rp
Most of the country receives a mean annual rainfall of Template:Convert.<ref name=tmd/> However, certain areas on the windward sides of mountains such as Ranong Province on the west coast of southern Thailand and eastern parts of Trat Province receive more than Template:Convert of rainfall per year.<ref name=tmd/> The driest areas are the leeward sides of the central valleys and the northernmost portion of south Thailand, where mean annual rainfall is less than Template:Convert.<ref name=tmd/>
Most of Thailand (north, northeast, central, and east) has dry weather during the northeast monsoon and abundant rainfall during the southwest monsoon.<ref name="tmd" />Template:Rp In the southern parts of Thailand, abundant rainfall occurs in both the northeast and southwest monsoon seasons, with a peak in September for the western coast and a peak in November–January on the eastern coast.<ref name="tmd" />Template:Rp
Northern vs southern climate
The tropical savanna climate in Northern Thailand vs the tropical monsoon climate in Southern Thailand has notable differences. The average temperature in Phuket (Southern Thailand) is warmer than Chiang Mai (Northern Thailand) year-round. However, Phuket has more rainy days and rainfall per month than Chiang Mai.
| Month | J | F | M | A | M | J | J | A | S | O | N | D | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Chiang Mai | Max Temp Av. | 29 | 32 | 34 | 36 | 34 | 32 | 31 | 31 | 31 | 31 | 30 | 28 | |
| Min Temp Av. | 13 | 14 | 17 | 22 | 23 | 23 | 23 | 23 | 23 | 21 | 19 | 15 | ||
| hours/day | 9 | 10 | 9 | 9 | 8 | 6 | 5 | 4 | 6 | 7 | 8 | 9 | ||
| mm/month | 7 | 11 | 15 | 50 | 140 | 155 | 190 | 220 | 290 | 125 | 40 | 10 | ||
| days/months | 1 | 1 | 2 | 5 | 12 | 16 | 18 | 21 | 18 | 10 | 4 | 1 | ||
| Phuket | Max Temp Av. | 31 | 32 | 33 | 33 | 31 | 31 | 31 | 31 | 30 | 31 | 31 | 31 | |
| Min Temp Av. | 23 | 23 | 24 | 25 | 25 | 25 | 25 | 24 | 24 | 24 | 24 | 24 | ||
| hours/day | 9 | 9 | 9 | 8 | 6 | 6 | 6 | 6 | 5 | 6 | 7 | 8 | ||
| mm/month | 35 | 40 | 75 | 125 | 295 | 265 | 215 | 246 | 325 | 315 | 195 | 80 | ||
| days/months | 4 | 3 | 6 | 15 | 19 | 19 | 17 | 17 | 19 | 19 | 14 | 8 | ||
| Reference: "Saisons et climats 2003" Hachette Template:ISBN | ||||||||||||||
Bangkok
The capital Bangkok has a tropical savanna climate (Aw) as per the Köppen climate classification. The Asian monsoon system influences the city's three seasons: summer (hot), rainy, and winter (cool). The winter is rarely below Template:Convert: circa Template:Convert in December to Template:Convert in April. The annual average temperature is Template:Convert.
The summer begins in mid-February and it's usually dry with occasional storms.<ref>Template:Cite web</ref> The rainy season is caused by the southwest monsoon around mid-May. September is the wettest month with around Template:Convert rainfall. The cool northeast monsoon causes the winter season from mid-October till mid-February.
Bangkok's urban heat island causes a temperature increase of Template:Convert during daytime and Template:Convert at night.<ref>Template:Cite journal</ref> Bangkok metropolis' highest temperature was Template:Convert on 7 May 2023.<ref name="CNN">Template:Cite news</ref> and the lowest Template:Convert in January 1955.<ref name="extreme minimum">Template:Cite web</ref>Template:Weather box
Natural resources
Land resources
- Tin, rubber, natural gas, tungsten, tantalum, timber, lead, fish, gypsum, lignite, fluorite, arable land.
Land use
- Arable land: 30.7%
- Permanent crops: 8.8%
- Other: 60.5% (2011)
Land ownership
Pattamawadee Pochanukul, a lecturer from the Faculty of Economics at Thammasat University, estimates that about 59% of all arable land in Thailand belongs to the state. Template:As of the Treasury Department owned 176,467 plots of land, consisting of about 9.9 million rai (15,769.6 km2).<ref>Template:Cite web</ref> The Ministry of Defence owns about 2.6 million rai (4,230 km2) or about 21.2% of total public land. Information from the Office of the National Anti-Corruption Commission (NACC) shows that members of the house of representatives in 2013 owned a total of 35,786 rai of land (about 57.3 km2).<ref>Template:Cite news</ref>
Irrigated land
- Total: 64,150 km² (2007)
Marine resources

Thailand has the world's 64th largest exclusive economic zone (EEZ), with an area of Template:Convert.<ref name="searoundus">Template:Cite web</ref><ref name=":12">Template:Cite web</ref> It claims an EEZ of Template:Convert from its shores, which has long coastlines with the Andaman Sea and Strait of Malacca to the west and the Gulf of Thailand to the east, although all of its EEZ is limited by maritime boundaries with neighboring countries. Circa 3/4th of the coastline around the Gulf of Thailand is part of Thailand.
Inland fishery
Over 150 fish species have been identified in catches from inland waters. 20 of these are economically important.<ref name=":6" /> The most common fish is the carp (represented by Puntius gonionotus, Puntioplites proctosyzron, Cirrhinus jullieni, Osteocheilus hasselti, Labiobarbus lineatus, Morulius chrysophekadion etc).<ref name=":6" /> The favorite fish of Thai people are 2 species of Snakehead (fish) called Channa striata and Channa micropeltes.<ref name=":6" /> The main catfish species are Clarias batrachus, C. microcephalus, Pangasius sutchi, P. larnooudii, P. siamensis, Kryptopterus pogon and Ompok bimaculatus.<ref name=":6" /> Corcia siamensis is the only representative of the clupeidae family.<ref name=":6" />
| Inland fishery resources of Thailand | ||
|---|---|---|
| Resource | Number | Area (ha) |
| Rivers and canals | 47 | 120000 |
| Natural lakes and swamps | 8000 | 300000 |
| Large reservoirs | 21 | 292590 |
| Medium and small reservoirs | 1745 | 425500 |
| Village ponds | 4947 | 25676 |
| Brackish water lakes | 1 | 96000 |
| Other public waters | 10859 | 143000 |
| Total | 1285420 | |
| Source: modified from Pawaputanon, 1992<ref name=":6">Template:Cite web</ref> | ||
Total renewable water resources
- Total: 438.6 km3 (2011)
Energy
In 2014, 75% of Thailand's electricity production was fueled by natural gas.<ref name=":1">Template:Cite web</ref> Coal-fired power plants produced an additional 20% of the electricity, with the remainder coming from biomass, hydropower, and biogas.<ref name=":1" />
Thailand produces about a third of the oil it consumes. It is the second-largest oil importer in Southeast Asia. Thailand is a major producer of natural gas, with reserves of at least 3 trillion cubic meters. After Indonesia, it is the largest coal producer in Southeast Asia, but it needs to import more coal to meet domestic demand.
Biota
Fauna
The biogeographic realm is part of the Indomalayan realm, spanning the Indochina and Sunda subrealms.[70] According to ONEP (2007), there are 302 recorded mammal species, 982 bird species, 350 reptile species, 137 amphibian species, and 2,820 fish species (720 freshwater fish speciesTemplate:Sfn).Template:Sfn The conservation status of 1,196 of these species was assessed in 2005, and 116 mammal species, 180 bird species, 32 reptile species, 5 amphibian species, and 215 fish species were listed as threatened.Template:Sfn Circa 264 mammal species in Thailand are on the IUCN Red List.
The elephant is a representative animal, and white elephants are considered symbols of kingship, have been featured on the national flag, and are considered to be the incarnation of Buddha in Buddhism, which is practiced by the majority of the population.<ref name="thai-elephant" /> At the beginning of the 20th century, there were approximately 100,000 elephants in captivity, but as of 2023, the wild population had declined to approximately 2,250 and the captive population to approximately 2,400. The central government has taken measures to protect elephants, such as opening conservation facilities and dedicated hospitals.<ref name="thai-elephant" /> See also elephants in Thailand. Water buffalo and bulls were also used as working animals, but by the 1980s, due to the diversification of transportation methods, they were rarely used as working animals.<ref name="Britannica2" />
Flora
The phytochorion belongs to the Paleotropical kingdom. It is estimated that approximately 1,900 genus and 10,000 species of vascular plants inhabit the region, of which about 10% are considered endemic.Template:Sfn Santisuk et al. (2006) lists a total of 1,407 species distributed in Thailand, including 921 species of dicotyledonous plants, 417 species of monocotyledonous plants, 42 species of ferns, and 27 species of gymnosperms.Template:Sfn
Major tree species include those of the Dipterocarpaceae family and teak,<ref name="Britannica3" /> as well as species from the Diospyros genus, Artocarpus genus, Lagerstroemia genus, and in mangrove forests, species from the Rhizophoraceae and Meliaceae families.Template:SfnTemplate:Sfn
Notable species native to Thailand
These are notable flora and fauna that live in their natural habitats of Thailand.<ref name=":8">Template:Cite web</ref>
Template:Static row numbersTemplate:Static row numbers
Environmental issues

Environmental concerns
- Natural hazards: Land subsidence in Bangkok, resulting from the depletion of the water table; droughts (see also 2004 Indian Ocean earthquake and 2011 Thai floods). Thailand is highly exposed to the effects of climate change such as the rising sea levels and extreme weather events.<ref>Template:Cite book</ref>
- Drought: Droughts are a persistent feature of Thailand's climate. Droughts appear to be worsening according to the Thai Meteorological Department.<ref>Template:Cite news</ref><ref>Template:Cite web</ref> and drought hazard mapping.<ref name="tmd" />
- Air pollution
- Water pollution from organic and industry wastes
- Deforestation
- Soil erosion
- Wildlife populations threatened by illegal hunting
Agriculture impact
The unpredictability of precipitation, temperature changes and many other harmful events will intensify in the future.<ref name=":0">Template:Cite web</ref> This means that Thailand will have to face droughts in the middle of the rainy season, which will result in damage to young plants and flooding of rice fields.<ref name=":0" /> It is therefore imperative for Thailand to adapt as quickly as possible to these changes to protect its population on the one hand and, if it wishes, to maintain a monopoly on the export of rice and not suffer significant losses.<ref name=":0" /> Which would ultimately have a huge impact on the country's economy.<ref name=":0" /> Particularly with the fluctuation in the price of rice, due to uncertainties, which prevents farmers from increasing their income.<ref name=":0" />
International environmental agreements
- Party to: biodiversity, climate change, climate change-Kyoto Protocol, desertification, endangered species, hazardous wastes, marine life conservation, Ozone layer protection, tropical timber 83, tropical timber 94, wetlands
- Signed, but not ratified: Law of the Sea
Territorial disputes
History
Thailand shares boundaries with Cambodia, Laos, Malaysia, and Myanmar. The territories of China and Vietnam do not border Thailand, but they are within around 100 km distance.
Many parts of Thailand's boundaries follow natural features, such as the Mekong river.<ref name=":08" /> Most borders were stabilized and demarcated in the late 19th and early 20th centuries in accordance with treaties forced on Thailand and its neighbors by the British Empire and French Indochina.<ref name=":08" /> In some areas, however, exact boundaries, especially along Thailand's eastern borders with Laos and Cambodia, are still disputed.<ref name=":08" />
Cambodia
Template:See also Cambodia's disputes with Thailand after 1951 arose in part from ill-defined boundaries and changes in France's colonial fortunes.<ref name=":08" /> Recently, the most notable case has been a dispute over Preah Vihear submitted to the International Court of Justice, which ruled in favor of Cambodia in 1962.<ref name=":08" /> During the years that the Cambodian capital, Phnom Penh, was controlled by the Khmer Rouge regime of Pol Pot (1975 to 1979), the border disputes continued.<ref name=":08" />
Laos
Template:See also Demarcation is complete except for certain Mekong islets. The border is marked by the Mekong: at high water during the rainy season, the centre line of the current is the border, while during low water periods, all islands, mudbanks, sandbanks, and rocks that are revealed belong to Laos.
Malaysia
Template:See also In contrast to dealings with Cambodia, which attracted international attention, boundary disputes with Malaysia are usually handled more cooperatively.<ref name=":08" /> Continuing mineral exploration and fishing, however, are sources of potential conflict.<ref name=":08" /> One segment at the mouth of the Golok River remained in dispute with Malaysia as of 2023, along with a section of the continental shelf in the Gulf of Thailand.<ref>Template:Citation</ref>
Myanmar
Sovereignty over three Andaman Sea islands remains disputed. The standing agreement, negotiated in February 1982, left undetermined the status of Ginga Island (Ko Lam), Ko Kham, and Ko Ki Nok at the mouth of the Kraburi River (Pakchan River). Subsequent negotiations in 1985, 1989, and 1990 made no progress. The two parties have designated the islands as "no man's land". Ongoing tensions in the area resulted in minor clashes in 1998, 2003, and 2013.<ref>Template:Cite news</ref>
See also
Notes
References
External links
Template:Thailand topics Template:Geography of Asia Template:Asia topic








