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[[File:Koppen World Map Cwa Cfa.png|thumb|right|upright=1.8| Warm temperate with hot summer climate zones of the world according to a modified Köppen climate classification that uses a threshold of for the coldest month.
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A humid subtropical climate is a Subtropics-temperate climate type, characterized by long and hot summers, and cool to mild winters. These climates normally lie on the southeast side of all continents (except Antarctica), generally between 25° and 40° and are located poleward from adjacent tropical climates, and equatorward from either humid continental (in North America and Asia) or (in other continents). It is also known as warm temperate climate in some climate classifications.
Under the Köppen climate classification, Cfa and Cwa climates are either described as humid subtropical climates or warm temperate climates. This climate features mean temperature in the coldest month between (or ) and and mean temperature in the warmest month or higher. However, while some climatologists have opted to describe this climate type as a "humid subtropical climate", Köppen himself never used this term. The humid subtropical climate classification was officially created under the Trewartha climate classification. In this classification, climates are termed humid subtropical when they have at least 8 months with a mean temperature above .
While many subtropical climates tend to be located at or near coastal locations, in some cases, they extend inland, most notably in China and the United States, where they exhibit more pronounced seasonal variations and sharper contrasts between summer and winter, as part of a gradient between the hotter tropical climates of the southern coasts and the colder continental climates to the north and further inland. As such, the climate can be said to exhibit somewhat different features depending on whether it is found inland, or in a maritime position.
Rainfall often shows a summer peak especially where storms reaching the level of are well developed, as in Southeast Asia and South Asia. Other areas have a more uniform or varying rainfall cycles but consistently lack any predictably dry summer months unlike Mediterranean climates (which lie at similar latitudes but, in most continents, on opposite coasts). Most summer rainfall occurs during thunderstorms that build up due to the intense surface heating and strong subtropical sun angle. Weak that move in from adjacent warm tropical oceans, as well as occasional Tropical cyclone often contribute to summer seasonal rainfall peaks. Winter rainfall (and occasional snowfall, especially near the poleward margins) is often associated with large storms in the westerlies that have fronts that reach down into subtropical latitudes.
Under the Holdridge life zones classification, the subtropical climates have a biotemperature between the frost or critical temperature line, (depending on locations in the world) and , and these climates are humid (or even perhumid or superhumid) when the potential evapotranspiration (PET) ratio (= PET / Precipitation) is less than 1. The climate of Carpathian Region in the 20th century based on the original and modified Holdridge life zone system In the Holdridge classification, the humid subtropical climates of the Koppen system coincide more or less with the subtropical and warm temperate life zones.
Cwa: C = Mild temperate w = Dry Winter a = Hot Summer
The climate is also found in the narrow coastal sections of southern and eastern South Africa, primarily in KwaZulu-Natal and the Eastern Cape provinces. South Africa's version of this climate features heavy oceanic influences resulting in generally milder temperatures. This is particularly evident in its winters when temperatures do not drop as low as in many other regions within the humid subtropical category.
The influence of the strong Siberian anticyclone in East Asia brings colder winter temperatures than in the humid subtropical zones in South America, and Australia. The isotherm reaches as far south as the valleys of the Yellow River and Wei River rivers, roughly latitude 34° N. At Hainan Island and in Taiwan, the climate transitions from subtropical into tropical. In most of this region, the winter monsoon is very well developed, as such eastern Asian humid subtropical zones have a strong winter dry season and heavy summer rainfall.
Only in inland areas below the Yangtze River and coastal areas between approximately the Huai River and the beginning of the coast of Guangdong is there sufficient winter rainfall to produce a Cfa climate; even in these areas, rainfall and streamflow display a highly pronounced summer peak, unlike other regions of this climate type. Drought can be severe and often catastrophic to agriculture in the Cwa zone.
The only area where winter precipitation equals or even exceeds the summer rain is around the San'in region at the western coast of Japan, which during winter is on the windward side of the westerlies. The winter precipitation in these regions is usually produced by low-pressure systems off the east coast that develop in the onshore flow from the Siberian high. Summer rainfall comes from the East Asian Monsoon and from frequent . Annual rainfall is generally over , and in areas below the Himalayas can be much higher still.
In Bangladesh, humid subtropical climates are commonly present in the northern half (north of Dhaka). Cities like Rajshahi, Rangpur, Saidpur and Dinajpur in the North Bengal feature the monsoon variant ( Cwa), where rainfall peaks at the monsoon season. Closely resembling the climate patterns of neighboring Northern India, this region shows a distinct three season pattern- relatively dry and very hot summer (March- early June), extremely wet, cooler Monsoon season (June- September), and mild, foggy winter (Late October- February).
Humid subtropical climates can also be found in Nepal. However, the Nepalese version of the climate generally does not feature the extreme hot spells that are commonplace for many other South Asian locations with this climate. In Nepal cities such as Kathmandu, Pokhara, Butwal, Birgunj and Biratnagar feature this iteration of the climate.
In South Asia, humid subtropical climates generally border on continental climates as altitude increases, or on winter-rainfall climates in western areas of Pakistan and northwestern India (e.g. Peshawar in northwestern Pakistan or Srinagar in the Kashmir Valley in India, where the primary precipitation peak occurs in March, not July or August). Further east, in highland areas with lengthier monsoons such as Nepal, seasonal temperature variation is lower than in the lowlands.
Southeast Asian locations with these climates can feature cool temperatures, with lows reaching during the months of December, January, and February. Unlike a good portion of East Asian locations with this climate however, most of Southeast Asia seldom experiences snowfall. These areas tend to feature hot and humid summers and cool and wet , with mean temperatures varying between in summer.
In Western Asia, the climate is prevalent in the Gilan, Māzandarān and Golestan Provinces of Iran, in parts of the Caucasus, in Azerbaijan and in Georgia wedged between the Caspian Sea and Black Sea seas and coastal (Black Sea) Turkey, albeit having more oceanic influence.
Annual rainfall ranges from around at Gorgan to over at Bandar-e Anzali, and is heavy throughout the year, with a maximum in October or November when Bandar-e Anzali can average in one month. Temperatures are generally moderate in comparison with other parts of Western Asia. During winter, the coastal areas can receive snowfall, which is usually of a short duration.
In Rasht, the average temperature in July and August is around but with near-saturation humidity, whilst in January and February it is around . The heavy, evenly distributed rainfall extends north into the Caspian coastal strip of Azerbaijan up to its northern border but this climate in Azerbaijan is, however, a Cfb/ Cfa ( Oceanic climate/ Humid subtropical climate) borderline case.
Western Georgia (Batumi and Kutaisi) in the Colchis and the northeast coast of Turkey (Giresun), have a climate similar to that of Gilan and Mazandaran in Iran and very similar to that of southeastern and northern Azerbaijan. Temperatures range from in summer to in winter and rainfall is even heavier than in Caspian Iran, up to per year in Hopa (Turkey). These climates are a Cfb/ Cfa ( Oceanic climate/ Humid subtropical climate) borderline case.
Under Köppen's climate classification, this zone includes locations further north, primarily Virginia, Kentucky, the lower elevations of West Virginia, Maryland, Delaware, Washington, D.C., southeastern and the lower elevations of southwestern Pennsylvania, central and southern portions of New Jersey, and Downstate New York. It can also be found in the lower Midwest, primarily in the central and southern portions of Kansas and Missouri and the southern portions of Illinois, Indiana and Ohio.
In Mexico, there are small areas of Cfa and Cwa climates. The climate can be found in small areas scattered around the northeastern part of the country, in proximity to the Gulf of Mexico. Other areas where the climate can be found is in the high elevations of Trans-Mexican Volcanic Belt and Sierra Madre Oriental. Despite being located at higher elevations, these locations have summers that are too warm to qualify as a subtropical highland climate. Guadalajara's climate is a major example of this.
Outside of isolated sections of Mexico, the southernmost limits of this climate zone in North America lie just north of South Florida and around southern coastal Texas. Cities at the southernmost limits, such as Tampa and Orlando and along the Texas coast around Corpus Christi down toward Brownsville generally feature warm weather year-round and minimal temperature differences between seasons. In contrast, cities at the northernmost limits of the climate zone such as New York, Philadelphia and Louisville feature hot, humid summers and chilly winters. These areas have average winter temperatures at the coldest limit of climates classed as humid subtropical. The climate can also be found in small areas scattered around the northeastern part Mexico, in proximity to the Gulf of Mexico.
Snowfall varies greatly in this climate zone. In locations at the southern limits of this zone and areas around the Gulf Coast, cities such as Orlando, Tampa, Houston, New Orleans, and Savannah rarely see snowfall, which occurs, at most, a few times per generation. In Southern cities farther north or inland, such as Atlanta, Charlotte, Dallas, Memphis, Nashville, and Raleigh, snow only occasionally falls and is usually three inches or less. However, for the majority of the winter here, temperatures remain above or well above freezing. At the northernmost limits of this zone, cities such as New York City, Philadelphia, Baltimore, Washington, D.C., and Louisville typically see snowfall during the winter, with occasional heavy snowstorms. Still, average temperatures during a typical winter hover just above freezing at these locations.
Precipitation is plentiful in North America's humid subtropical climate zone – but with significant variations in terms of wettest/driest months and seasons. Much of the Upland South, including Tennessee, Kentucky, and the northern halves of Mississippi and Alabama, tends to have a winter or spring (not summer) precipitation maximum. Closer to the South Atlantic and Gulf coasts, there is a summer maximum, with July or August usually the wettest month – such as in Jacksonville, Charleston, Mobile, New Orleans, and Virginia Beach. A semblance of a monsoon pattern (dry winters/wet summers) is evident along the Atlantic coast from the Chesapeake Bay region and the Outer Banks south to Florida. The seasonal monsoon is much stronger on the Florida peninsula, as most locations in Florida have dry winters and wet summers.
In addition, areas in Texas that are slightly inland from the Gulf of Mexico, such as Austin and San Antonio that border the semi-arid climate zone, generally see a peak of precipitation in May, a drought-like nadir in mid-summer and a secondary, if not equal, precipitation peak in September or October. Areas further south along South Texas' Gulf Coast (Brownsville), which closely border Tropical climate, typically have a strong September precipitation maximum, and a tendency toward dry conditions in winter with rain increasing in spring, with December or January often the driest months.
The Cwa climate occurs in parts of tropical highlands of Minas Gerais, Rio de Janeiro, Mato Grosso do Sul and near the Andean highland in northwestern Argentina. These highland areas feature summer temperatures that are warm enough to fall outside the subtropical highland climate category.
From Newcastle, approximately northeast of Sydney, the Cfa zone would extend to inland New South Wales, excluding the highland regions (which have an oceanic climate), stretching towards Dubbo to the northwest and Wagga Wagga to the south, ending at the New South Wales/Victoria border (Albury-Wodonga). To note, these places would have characteristics of the semi-arid and/or Mediterranean climates. Furthermore, the inland Cfa climates generally have drier summers, or at least summers with low humidity.
Extreme heat is more often experienced in Sydney than in other large cities in Australia's Cfa zone, especially in the western suburbs, where highs over are not uncommon. Frost is prevalent in the more inland areas of Sydney, such as Richmond. Average annual rainfall in the Sydney region ranges between . (2025). 9781876334680, Reed New Holland. ISBN 9781876334680
There is usually a distinct summer rainfall maximum that becomes more pronounced moving northwards. In Brisbane, the wettest month (February) receives five times the rainfall of the driest month (September). Temperatures are very warm to hot but are not excessive: the average maximum in February is usually around and in July around . Frosts are extremely rare except at higher elevations, but temperatures over are not common on the coast.
North of the Cfa climate zone there is a zone centred upon Rockhampton which extends north to the Köppen Cwa classified climate zone of the Atherton Tablelands region. This region has a very pronounced dry winter period, with often negligible rainfall between June and October. Winter temperatures generally only fall slightly below , which would classify the region as a tropical savanna, or Aw, climate.
Annual rainfall within Australia's humid subtropical climate zone can reach as high as in coastal locations and is generally or above. The most intense 2-3 day rainfall periods that occur in this coastal zone however are the outcome of east coast lows forming to the north of a anticyclone. There can be great variation in rainfall amounts from year to year as a result of these systems. As an example at Lismore which lies in the centre of this zone, the annual rainfall can range from less than in 1915 to more than in 1950.
The climate of Lord Howe Island and Norfolk Island to the east of Australia is also Cfa, as is the climate of the Kermadec Islands to the northeast of New Zealand. Strong Pacific influences on these islands prevent extreme heat despite very mild winters.
The Po Valley, in Northern Italy, including major cities such as Milan, Turin, Bologna, and Verona, has a humid subtropical climate, featuring hot, humid summers with frequent thunderstorms; winters are foggy, damp and chilly, with sudden bursts of frost. Places along the shores of Lake Maggiore, Lake Lugano, Lake Como (Como and Verbania in Italy and Lugano and Locarno in Switzerland) have a humid subtropical climate with a distinctively high amount of rainfall during summer. In France, the climate is found in parts of the Garonne (city of Toulouse) and in the Rhône Valley, including the cities of Lyon and Valence. Due to climate change, some cities on the Balkan peninsula and in the Pannonian Basin such as Belgrade, Novi Sad, Niš and Budapest are now just warm enough to be categorized as such. At 48°N, the urban core of Vienna, in Austria and Bratislava, in Slovakia, lie on the northern limit of the humid subtropical zone.
The coastal areas in the northern half of the Adriatic Sea also fall within this climate zone. The cities include Trieste, Venice, and Rimini in Italy, Rijeka and Split in Croatia, Koper in Slovenia and Kotor in Montenegro. Other Southern European areas in the Cfa zone include the central valleys and coast of Catalonia of Girona and Barcelona in Spain, some on the north-east of Spain (Huesca), West Macedonia in Greece (Kozani).
Along the Black Sea coast of Bulgaria (Varna), coast of Romania (Constanța and Mamaia), Sochi, Russia and Crimea, have summers too warm (> mean temperature in the warmest month) to qualify as oceanic, no freezing month, and enough summer precipitation and sometimes humid conditions, where they would be fit to be classed under Cfa, though they closely border the humid continental zone due to colder winters. All these areas are subject to occasional, in some cases repeated snowfalls and freezes during winter.
In Central Europe, a small area of humid subtropical climates are located in transitional areas between the oceanic and continental climates in areas where higher summer temperatures do not quite qualify it for inclusion in the Oceanic climate schema and mild winters do not allow their inclusion into continental climates. Average summer temperatures in areas of Europe with this climate are generally not as hot as most other subtropical zones around the world. Urban examples include Bratislava, Budapest, and the Innere Stadt of Vienna.
In the Azores, some islands have this climate, with very mild and rainy winters (>) and no snowfall, warm summers (>) but with no dry season during the warmest period, which means that they can neither be classified as oceanic climate, nor as Mediterranean, only as humid subtropical, as with Corvo Island.
In many other climate classification systems outside of the Köppen, most of these locations would not be included in the humid subtropical grouping. The higher summer precipitation and poleward flow of tropical air-masses in summer are not present in Europe as they are in eastern Australia or the southern United States. Many of these locations in Central and Southern Europe are considered oceanic climate by Trewartha's classification.
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