Climate in United States

Being a huge country, the contiguous United States is home to a wide variety of climates. However, in general it has a continental climate, with cold winters (often frigid) and hot summers (sometimes very hot), with a different season duration depending on latitude and distance from the sea.
There are, however, some exceptions: on the west coast overlooking the Pacific Ocean, the climate is cool and damp in the northern part and Mediterranean in the southern part; on the coast of the Gulf of Mexico, the climate is mild in winter and hot and muggy in summer, while in Florida, it is almost tropical; the mountainous areas are cold in winter and cool to cold even in summer; and finally, there are deserts which are mild in winter and scorchingly hot in summer.

Since there are no obstacles to cold air masses from Canada, almost all of the country can experience sudden cold waves in winter, but they have different intensity and duration depending on area. Cold spells last a few days in the south, where the temperature drops a few degrees below freezing (0 °C or 32 °F) in winter, while they are intense and sometimes long in inland areas, in the highlands and in the north-east.
Heat waves in summer can be intense as well, especially in inland areas.

As regards to precipitation (rain or snow), in general, the western half of the country is more arid than the eastern one, with the exception of the north-central coast of the Pacific, which is rainy.

The Western United States are mostly occupied by mountains and plateaus, with vast arid and desert areas.
On the other hand, the central-eastern part is mostly flat or covered by hills and low mountains, and its climate is generally more humid and rainy. Given the vastness of the territory, the climatic differences are remarkable here as well.
In the central-eastern part, clashes of air masses are remarkable and frequent, making the climate unstable in most of the territory, and meteorological phenomena may be violent (storms, hail, blizzards, tornadoes). Air masses coming from Canada are cold and dry (but pick up moisture when passing over the Great Lakes), while those from the Gulf of Mexico are warm and moist.
The Great Plains experience higher temperature variations, but are also less humid and rainy than the East Coast, especially in winter.

In the following map, we can see the climate zones in the United States.

Index

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• West Coast - Seattle, San Francisco, Los Angeles, San Diego
• Deserts - Las Vegas, Phoenix, Tucson
• Plateaus - Salt Lake City, Denver, Albuquerque
• Rocky Mountains
• Center-east: cold continental climate - Duluth, Fargo
• Center-east: continental climate - Minneapolis, Chicago, Des Moines
• Center-east: temperate continental climate - Cincinnati, Boston, New York, Washington
• Center-east: temperate climate - Dallas, Memphis, Atlanta
• Center-east: subtropical climate - Houston, New Orleans
• Center-east: tropical climate - Miami
• Center-east: hurricanes
• Center-east: tornadoes
• When to go
• What to pack
• Climate data

West Coast

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In the north-western states (Washington, Oregon), the weather is cool and rainy along the west coast and along the west-facing slopes, in cities like Seattle, Portland, and Eugene. Average temperatures in winter are about 3/5 °C (37/41 °F), but every so often, cold air masses from Alaska can arrive here.
In Seattle, the average temperature ranges from 6 °C (43 °F) in January to 19.5 °C (67 °F) in July and August.
Rainfall is most abundant from November to January, though it's common for most of the year, except in summer. In fact, in July and August, the weather is pleasant and quite sunny, with cool nights and some morning fogs. While rainfall is frequent, snow is rare.
The sea is cold all year round, and ranges in in Seattle from 8 °C (46.5 °F) in January to 13.5 °C (56 °F) in August.

Proceeding south, the west coast remains cool even in northern California and down to San Francisco, but winter becomes progressively milder, and cold spells become rarer, so that the climate begins to acquire Mediterranean characteristics.

In San Francisco and in the cities located in the bay of the same name, the climate is mild, rainy in the winter months and sunny in the remainder of the year. Summer is particularly cool, often foggy in the morning, and the temperatures are similar to those of London. But luckily, the sun comes out in late morning, and it usually shines for the rest of the day. Sometimes, however, it can get hot even in San Francisco, when the wind blows from inland.
Near San Francisco too, the sea is cold all year round, in fact its temperature reaches a maximum of 14/14.5 °C (57/58 °F) from August to October.



Continuing south along the coast of California, the temperature continues to rise, and the climate becomes milder, very pleasant, spring-like and sunny all year round, down to the border with Mexico. This happens because a cool current flows along the coast of California, which is able to make the climate mild and to hinder rain cloud formation, although it can generate low clouds and coastal fogs. But away from the coast, the heat in summer is more intense. For example, the summer temperatures are considerably higher in the Sacramento Valley than on the coast: in July and August, highs in cities like Redding, Stockton, Fresno, Bakersfield are around 35/37 °C (95/99 °F), while on the coast, they do not go above 20 °C (68 °F)!

Going further south, in the Los Angeles area, the climate is pleasantly warm for most of the year: this is perhaps one of the finest climates in the world, even though it only applies to the coast and the surrounding areas.
In winter, the maximum temperatures are very mild, around 20/21 °C (69/71 °F). In July, the average maximum temperature is 23.5 °C (74.5 °F) in Santa Barbara (on the coast to the west of Los Angeles) and it's already 29 °C (84 °F) in downtown Los Angeles, while 40 kilometers (25 miles) to the east, in Pomona, still in the Los Angeles conurbation (which is very extended), it reaches 33 °C (91 °F). In San Bernardino, 45 km (30 mi) more to the east, the average reaches 36 °C (97 °F), while in Palm Springs, 70 km (45 miles) to the south-east, and located in the desert, it is as high as 42 °C (108 °F).
In Los Angeles, the sun shines throughout the year, except during the short periods of bad weather which can occur in winter: movies and tv series filmed in Hollywood, where the sun always shines, do not lie.
It rains (not much) from mid-November to mid-April, and almost never in the rest of the year.
On the coast near Los Angeles, the sea is very cool even in summer, however, it reaches 18.5 °C (65 °F) in August and September.



The only disturbing element in the climate of this region is represented by the Santa Ana, a hot and very dry wind, which can affect the coastal regions of Southern California. This wind is often accompanied by dust, and it's also capable of generating fires. More frequent in autumn and winter, it can occur in all seasons, and usually lasts a few days.

The islands off the coas of California (Channel Islands) are very mild, sunny, and semi-desert. In winter, they are as mild as the smaller islands of the Mediterranean, while in summer, they are cool, with highs around 22 °C (72 °F). In addition, owing to the cool current, cloud banks can form above the sea in summer, so the sky can be overcast.

South of Los Angeles, and near the border with Mexico, we find San Diego, where the climate is similar to that of the L.A. coast.

The deserts

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In the United States, there are four desert areas, contiguous to each other. The northernmost is the Great Basin, an area that covers most of Nevada and western Utah, but since it has cold winters, it will be discussed later, along with the highlands. Here, on the contrary, we will talk about the hot deserts.

Mojave Desert

As previously mentioned, about 150 kilometers (95 miles) south-east of Los Angeles, we find Palm Springs, a desert city, scorchingly hot in summer. The desert that extends through south-eastern California, southern Nevada and south-western Arizona is called Mojave Desert: this is the most typical type of desert, with sunshine for most of the year, low rainfall, around 100 mm (4 in) per year or less, concentrated in winter and virtually absent in summer.

The hottest areas of the desert are the valleys that lie around sea level or even below, such as Death Valley, a depression at 85 meters (280 feet) below sea level. Here, there's a mild winter, with highs around 19/20 °C (66/68 °F) and lows around 5 °C (41 °F), and a long, scorching summer, with average highs around 42/47 °C (108/117 °F). Death Valley is the hottest place in North America, and one of the hottest in the world: here, the highest recorded temperature is an incredible 54.4 °C (130 °F)!



At higher altitudes, the weather remains hot in summer, but it's more bearable, while winter nights can be cold. In Las Vegas, Nevada, at 650 meters (2,100 ft) above sea level, winter is mild during the day, around 14/15 °C (57/59 °F), but with possible slight frosts at night. Snow is very rare, though in winter, the mountains surrounding the city are often covered with snow. Summer is hot, with highs generally around 40 °C (104 °F).
Every so often, a thunderstorm may break out during summer, but for the rest, the sun almost always shines: in Las Vegas, there are as many as 3,820 hours of sunshine per year, even more than in Los Angeles (3,250 hours) and in San Francisco (3,060 hours).

Sonoran Desert

Further south, between the south-eastern tip of California and the southwestern part of Arizona, we find the Sonoran Desert. Here, the rainfall is slightly higher, between 100 and 250 mm (4 and 10 in) per year, and there's a maximum in summer due to moist air coming from the Gulf of California, which creates a kind of "little summer monsoon". This is the area where the saguaro, the giant cactus, is found. Let there be no mistake: the weather is still sunny for most of the year, but we cannot exclude some thunderstorms, sometimes even strong, in summer.

Phoenix, Arizona, at 340 meters (1,100 feet) above sea level, is located at the edge of the area. Here, winter is mild, with cold nights but spring-like days, around 18/20 °C (64/68 °F), while summer is scorchingly hot, around 40/41 °C (105/107 °F) during the day. Phoenix is famous in the United States for being a very hot city. The sun almost always shines (up to 3,875 hours per year), but in summer, from July to September, every so often, a thunderstorm can break out, and the wind can cause sandstorms.

In Tucson, Arizona, located further south, at almost 800 meters (2,600 feet) above sea level, the peak of the rainfall in summer is even more evident: on average, 55 mm (2.2 in) of rain fall in July, 50 mm (2 in) in August and 35 mm (1.4 in) in September. The maximum temperature is highest in June, 38.5 °C (101 °F) on average, while later it drops slightly, to 38 °C (100 °F) in July and to 37 °C (99 °F) in August, when, however, the humidity slightly increases.

Chihuahuan Desert

Continuing east, in south-eastern Arizona, southern New Mexico and the westernmost part of Texas, we find the Chihuahuan Desert.
Of course, the sun shines even here for most of the year, but the higher altitude, between 600 and 1,500 meters (2,00 and 5,000 feet), makes the climate milder. In winter, lows are around freezing (0 °C or 32 °F) or a few degrees below, while highs range between 15 °C and 18 °C (59 and 64 °F), but sometimes, during cold waves, it can even snow; spring can be windy, and in summer, highs hover around 35 °C (95 °F). Here, too, there's a peak in the rainfall in summer, between July and September, due to thunderstorm cells coming from the Gulf of California, which can sometimes cause floods.
Two cities that are located in this climatic zone are El Paso, Texas, at 1,200 meters (3,900 feet) above sea level on the border with Mexico, and Roswell, New Mexico, at 1,100 meters (3,600 feet).
The Chihuahuan Desert is located in the southernmost part of the plateaus of the western United States (which we will deal with in the following paragraph), although temperatures are somewhat higher, and the little rainfall occurs especially in summer.

The plateaus

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East of the Pacific Coast, two mountain ranges, both parallel to the coast, the Cascade Range in the north and the Sierra Nevada in the south, isolate the interior of the continent from maritime influences. East of these mountain chains, we find the huge area of the Rocky Mountains, which cross the central-western United States from north to south.
In addition to the highest peaks and ranges, there is a wide area of plateaus and valleys at high altitude, where the climatic characteristics are quite similar: the winter is cold, with possible intense cold waves and snowfall, the summer is hot and sunny, with possible afternoon thunderstorms, there are significant temperature variations between night and day, precipitation is scarce, the air is limpid. In addition, there are sudden increases in temperature due to the Chinook, the warm wind that descends from the mountains and is able to melt snow in a short time.
Proceeding from north to south, the climate becomes progressively warmer, while there are also some local differences (as regards to precipitation as well) depending on altitude and slope exposure. In general, the southern highlands are the driest, but there are "rain shadow" areas also in the north.



In the states of Washington and Oregon, which, as we said before, are mild and rainy along the coast, the bulk of precipitation coming from the ocean is released on the Cascade Range.
To the east of this mountain range, there is an arid plateau, where the climate is continental, with wide temperature range between day and night. Total precipitation is scarce, though it is more abundant in winter, with possible heavy snowfalls. Strong waves of frost may occur in winter and also some heat waves in summer; the latter are less frequent than in the center-south.
In this area we find the cities of Spokane (located in the state of Washington), Eureka (Montana), Alturas (California), Boise (Idaho), Reno, (Nevada).

East of Nevada, in Utah, we find Salt Lake City, located at 1,300 meters (4,250 feet) above sea level, near the Great Salt Lake. Here, the average temperature ranges from -0.5 °C (31.5 °F) in January to 27.5 °C (81 °F) in July; therefore, summer is hot, with some scorching days, and also sunny.
Annual precipitation is not so scarce: 395 mm (15.5 in), with a maximum in spring and a minimum in summer. Between November and April, a lot of snow falls: 145 cm (55 in) on average. This city is located in a valley, and during winter, in periods of calm weather, pollutants accumulate in the air because of cold air stagnation.
East of the city, there are snowy mountains, where the ski resort of Park City is found. Alta, at an elevation of 2,600 meters (8,500 ft), is the second snowiest place in the United States, with its 13 meters (42.5 feet) of snow per year.



North-east of Utah, in the state of Wyoming we find Cheyenne, at an altitude of as high as 1,870 meters (6,135 feet), where the average temperature ranges from -2 °C (28 °F) in December to 21 °C (70 °F) in July. Here, too, precipitation is around 400 mm (16 in) per annum, with a maximum from May to August (mostly due to afternoon thunderstorms) and a minimum in winter. However, from late October to early May, snow falls (especially in March and April, when precipitation is higher than in winter), totalling 150 cm (60 in) on average. Being that this city lies on the eastern slope of the Rocky Mountains, the Chinook blows frequently, bringing warm and dry conditions. Hence, waves of frost can be intense, but do not last long. The sun frequently shines throughout the year.

South of Wyoming, in Colorado, we find Denver, which is located at 1,600 meters (5,250 feet) and has similar characteristics (sunshine, dry air, frequent Chinook, intense but short cold waves, wide temperature range between day and night), although it is a bit milder. The monthly average temperature ranges from -0.5 °C (31 °F) in December to 24 °C (75 °F) in July, when, however, nights are mild to cool and days are hot and sometimes scorching.

South of Colorado, we find New Mexico, whose largest city, Albuquerque is located at 1,600 meters (5,250 feet) of altitude. Here, we are at the edge of the Chihuahuan Desert, in fact, rainfall is scarce, 225 mm (9 in) per year, with a maximum between July and September due to the influence of the "little summer monsoon", which affects Arizona and New Mexico and of which we have already spoken.

Between Utah and Arizona, we find the Monument Valley, at 1,600 meters (5,250 feet) of altitude. Here, winter is cold, with an average in January around freezing. In contrast, summer is hot during the day, with maximum temperatures around 30/33 °C (86/91 °F), and cool nights. Precipitation is practically at desert levels, in fact, it is lower than 200 mm (8 in) per year, but at times, thunderstorms can break out, which may take tourists by surprise, creating sudden streams in the valleys.



In the Grand Canyon, Arizona, the climate varies with altitude. The south side is located at 2,100 meters (6,900 ft) above sea level, and has cold, snowy winters (but there may also be periods of good weather, with sunshine during the day and freezing temperatures at night) and warm summers, when days can be hot, but nights remain cool. Between July and September, some thunderstorms may break out in the afternoon, sometimes intense. The north side is located at an even higher altitude, around 2,500 meters (8,200 ft), so it's even colder, and it's covered by a coniferous forest.
But at the bottom, inside the deep gorges where the river Colorado flows, about 700 meters (2,300 feet) above sea level, the climate is very different, and it is similar to that of Las Vegas: desert and scorchingly hot for several months, with mild winters.



In Arizona, above 2,000 meters (6,500 feet), we find cities such as Flagstaff and Williams, where the climate is similar to the upper part (south side) of the Grand Canyon: the average temperature is around freezing in January and around 20 °C (68 °F) in July; snowfalls can occur, sometimes heavy, in winter, while there's a lot of sunshine for most of the year, and some afternoon thunderstorms in summer.

Rocky Mountains

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We have already talked about the parts of the mountain areas in which the climate is continental: here, we will talk about the areas where there is a cold mountain climate (Alpine) because of the altitude.
As mentioned, in the state of Washington, the mild Pacific currents release moisture as precipitation on the western slopes of the Cascade Range. Mount Rainier is the snowiest place in the United States, with 17 meters (55 feet) of snow per year!
At the highest altitudes, above 2,000 meters (6,500 feet), even in Arizona there are forests and ski resorts (such as the Apache National Forest and the Sunrise Park Resort).

The Yellowstone National Park, Wyoming, which has an average altitude of 2,400 meters (7,900 ft), has a subarctic climate, cold for most of the year. The temperature remains below freezing for months, and snowfalls are abundant. The coldest records are spectacular, below -40 °C (-40 °F).
In the summer months, the temperature is pleasant during the day, around 20/24 °C (68/75 °F), but it's still cold at night (a few degrees above freezing).
Precipitation, about 500 millimeters (20 inches) per year, is evenly spread over the seasons, and occurs in the form of snow for several months.

In the Rocky Mountains, we find ski resorts such as Vail and Aspen in Colorado, the aforementioned Park City in Utah, and those of the Sierra Nevada in California.



As regards to the Sierra Nevada, we can mention the Yosemite National Park, which has different climates depending on altitude, and the Sequoia National Park.

Center-east: cold continental climate

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In the northernmost part of the east-central United States (which includes the northern part of Montana, North Dakota and Minnesota, most of Wisconsin and Michigan, northern Pennsylvania, north-central New York state, the interior of Massachusetts, and the states of Vermont, New Hampshire and Maine), the climate is continental with long, cold, snowy winters and mild or pleasantly warm summers.
The average daily temperature in January is several degrees below freezing, from -15 °C (5 °F) to -3 °C (26.5 °F), while in July, it doesn't reach 22 °C (71.5 °F). Summer is a fairly rainy season because of afternoon thunderstorms in the west, and also because of the weather disturbances that can affect the areas of the Great Lakes and the east. However, the sun frequently shines. During summer, intense heat waves can occur, with peaks above 35 °C (95 °F), but they only last a few days.
Being that the climate of this area is inhospitable, no large cities are found.

In Duluth (Minnesota), the average temperature goes from -11.5 °C (11.5 °F) in January to 19.5 °C (67 °F) in July. So, the summer is not very warm.
Lake Superior approaches the freezing point in winter (but on colder winters, a thick layer of ice forms), while in summer, although it warms up considerably, it remains very cool, if not cold, for swimming.
In this area, precipitation is fairly scarce in the western part, where it's inferior to 500 millimeters (20 inches) per year, mainly because of the relatively dry winter, while it's more abundant in the Great Lakes region and in the north-east. In Duluth, precipitation amounts to 800 mm (31.5 in) per year.
As a consequence, snowfalls (which typically occur from late October to mid-April) are relatively less abundant in the west, where they amount to about 70 cm (27.5 in) per year in North Dakota, while they are definitely abundant around the Great Lakes and in the north-east: typically, they range from 150 to 250 cm (60 to 100 in), but they can even surpass 3 meters (120 in) in the Upper Peninsula.

In the area of the Great Lakes, winter snowfalls are more abundant along the coasts exposed to the north and west (because of a phenomenon called lake-effect snow, whereby cold winds, initially dry, pick up moisture over the lakes, and bring snowfall on the leeward shores). In Houghton, northern Michigan, on the shores of Lake Superior, snowfall amounts to 5 meters and 30 cm (208 inches) per year; in L'Anse, a little more to the south and 500 meters (1,600 feet) above sea level, it almost reaches 6 meters (20 feet) per year!

In the northeast, Mount Washington New Hampshire, 1,917 meters (6,289 feet) high, is constantly affected by disturbances generated by the clash between warm and cold air masses, and receives no less than 7 meters (23 feet) of snow per year.



In the western part of this area, that is to say in the northern part of the Great Plains, precipitation is scarcer, but the temperature changes are intense, and in summer it is more likely to get hot.

In Fargo, North Dakota, the average in January is -12.7 °C (9.1 °F), like in northern Sweden. The temperature drops below -18 °C (0 °F) for 50 days a year on average. Summer is warm: the average in July is 21.5 °C (70.5 °F), although nights remain typically cool.
Precipitation amounts to 610 mm (24 in) per year, with a minimum in winter and a maximum in early summer due to afternoon thunderstorms. Snowfall amounts to 130 cm (51 in) per year.

Along the east coast, in Portland, Maine, winter temperatures are higher, in fact, the average ranges from -4.5 °C (24 °F) in January to 21.5 °C (70.5 °F) in July. Annual precipitation is abundant, and amounts to 1,200 mm (47 in), well distributed throughout the year, though with a relative minimum in summer. Here, 175 cm (69 in) of snow fall per year.

Center-east: continental climate

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Further south of the area at the border with Canada, we find an area of the United States (which includes most of South Dakota and Nebraska, the entire state of Iowa, south-central Minnesota, and the north-central part of Illinois, Indiana and Ohio, plus a small portion of the northeast) where the climate is continental, and where the average temperature in January is below or equal to -3 °C (26.5 °F), while the summer is warm to hot, given that the average in July exceeds 22 °C (71.5 °F).

With an average January temperature of -9 °C (16 °F), Minneapolis, Minnesota, is colder than Moscow, Russia. In a typical year, from November to April, 130 cm (50 in) of snow fall. In the worst periods, the temperature can plunge to -35 °C (-31 °F). On the other hand, summer is quite hot: the average in July is 23.5 °C (74.5 °F). Precipitation, about 805 mm (31.5 in), is scarcer in winter and more abundant in summer, when it occurs mainly in the form of thunderstorm.

Further south, in Des Moines, Iowa, the average temperature ranges from -5.3 °C (22.5 °F) in January to 24.5 °C (76 °F) in July. On average, 94 cm (37 in) of snow fall each year.

On the coast of Lake Michigan, Chicago, known as the "Windy City", has cold winters, with freezing periods due to outbreaks of cold air from the Canadian Arctic region, but also some milder periods. The average in January is -3 °C (26.5 °F), but the temperature drops below -18 °C (0 °F) for an average of 4 nights per year. Snowfall amounts to about one meter (40 in) per year. Summers are warm to hot and humid, with thunderstorms in the afternoon, and also with possible heat waves.
The daily average in July is 25 °C (77 °F). During summer, the temperature exceeds 32 °C (90 °F) for 21 days on average.



Further east, in Detroit (Michigan), near the north shore of Lake Erie, the climate is similar to that of Chicago.
The coast of the state of New York overlooking Lake Erie and Lake Ontario has similar temperatures, but it's particularly snowy on account of the aforementioned lake-effect snow. In Cleveland (Ohio), 160 cm (63 in) of snow fall per year, while in Buffalo, snowfall reaches 240 cm (95 in). The temperatures are similar to those of Chicago, but summer is a bit milder because of the cooling effect of the lake, which here is more evident.
North of Buffalo, between Lake Erie and Lake Ontario, we find the Niagara Falls.

Center-east: temperate continental climate

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In this band (which includes most of Kansas and Missouri, the north of Oklahoma and Arkansas, north-central Tennessee, south-central Illinois, Indiana and Ohio, the states of Kentucky, Connecticut, Rhode Island, West Virginia, New Jersey, Delaware, the District of Columbia, the south of Pennsylvania, New York and Massachusetts, and most of Virginia), the climate is continental, but is more forgiving in winter, while it becomes definitely hot in summer. Winter is still cold, with an average in January ranging from -3 °C to 3 °C (26.5 to 37.5 °F); there can be cold waves, but they alternate with mild periods.
Summer is hot and sunny, especially in the western part, while it's a bit milder in the area of the Appalachian Mountains and along the east coast. Summer is a fairly rainy season, mainly because of afternoon thunderstorms, but in the central and eastern part, some weather fronts may also pass. In summer, heat waves can occur, sometimes intense, and unlike in the north of the country, they can be persistent.

In this area, several large cities are found.
Here too, the western part, that of the Great Plains, is less rainy than the central and eastern part, and is characterized by more intense temperature changes.

Kansas City is located in the Great Plains of the Midwest, near the geometric center of the United States. Here, winter is cold, and the average in January is -0.5 °C (31 °F). Summer is definitely hot, with an average in July of 27 °C (81 °F), and muggy too.
The amount of sunshine is great: 2,800 hours per year. Precipitation amounts to 1,000 mm (40 in) per year, and it's most abundant in late spring and summer, when it often occurs in the form of thunderstorm. On average, 28 cm (11 in) of snow fall per year.

Moving to the east, the climate of St. Louis (Missouri) is similar to that of Kansas City, while in Indianapolis (Indiana) and Cincinnati (Ohio) it is slightly milder, but also more humid.

The Appalachian Mountains are very snowy in winter, at least on the north-western slopes: snowfall is abundant especially on the north-facing elevations of West Virginia, where it amounts to about 150 cm (60 in) per year, and it's less abundant on those of Virginia, where it amounts to 50 cm (20 in) per year. The altitude tempers a bit the summer heat in the cities located at low-mountain elevations.
In this area we find the Great Smoky Mountains National Park.

On the east coast, the proximity to the sea makes the climate a bit more temperate, but it must be said that the prevailing currents come from inland, so the climate is still continental.



New York, despite being on the coast and at a relatively low latitude, 41° north, has a cold winter: the average in January is 0.8 °C (33.4 °F). Summer is hot and muggy, and the average in July is 25.3 °C (77.5 °F). The climate is perpetually unstable, in fact all kinds of weather may occur: clear or overcast, windy or calm, cold or warm, even within the same week.

Further to the north-east, Boston (Massachusetts), is a bit colder and snowier in winter: the average in January is -1 °C (30 °F), the annual amount of snow is 125 cm (49 in), and snow storms can be even worse than in New York. On the other hand, summer is a little milder: the average in July is 23.5 °C (74 °F).
Owing to the fact that the sea is colder, fog can sometimes occur in spring, while in summer, sea breezes are often effective in tempering the heat. Here too, heat waves may occur in summer, and there are frequent thunderstorms in the afternoon, sometimes accompanied by hail.

South of New York, Washington, the federal capital, is instead a bit warmer than the Big Apple: the average ranges from 3 °C (37.5 °F) in January to 27 °C (81 °F) in July.

Center-east: temperate climate

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In this belt (which includes the center and south of Oklahoma, the central part of Texas, south-central Arkansas, southern Tennessee, most of the states of Mississippi, Alabama, North and South Carolina, and north-central Georgia), winter is quite mild, in fact the average temperature in January is between 3 °C and 9 °C (37.5 and 48 °F).
However, since there are no obstacles blocking the cold currents from the north, cold waves, usually short-lived, are also possible at these latitudes.
In the north of this band, 15/20 cm (6/8 in) of snow still fall per year, while in the south, the snowfall average drops to about a few centimeters per year, which means that sometimes, it never snows for an entire winter (or maybe, more than one).
Summer, is long, hot and muggy, tropical-like, with afternoon thunderstorms, sometimes intense, especially in the central and eastern part. Oklahoma and north-central Texas are often oppressively hot, with an annoying combination of moisture and high temperature: highs range between 34 °C and 36 °C (93/97 °F), but they can remain around 40 °C (104 °F) for weeks. Further east, temperatures are a bit lower, in fact, highs are usually around 32/33 °C (90/91 °F), but relative humidity is even higher. After all, we are at the latitude of northern Africa, but south of this area, instead of the Sahara, there is the Gulf of Mexico, from which warm, moist air masses often arrive.
Precipitation drops below 1,000 mm (40 in) per year in the western area (Texas, Oklahoma), while it's quite abundant in the central-eastern part, where it reaches about 1,200/1,300 mm (47/51 in) per year. Spring is a very rainy season because of the conflict between air masses coming from the north, which are still cold, and subtropical air masses lying in the south. In spring, tornadoes may also occur (see below).
At this latitude, the westernmost part of Texas belongs to the Chihuahuan Desert, of which we have previously spoken.



In Dallas, the average temperature ranges from 7.7 °C (45.9 °F) in January to 30.2 °C (86.4 °F) in July. Annual precipitation amounts to 940 mm (37 in).

In Memphis, Tennessee, the average temperature ranges from 5.5 °C (42 °F) in January to 28 °C (82 °F) in July. Here, too, winter is mild, but there can be some short and intense waves of frost, accompanied with snow; on average, 12 cm (4.7 in) of snow fall per year.
Rainfall, much more abundant than in Dallas, amounts to 1,400 mm (55 in) per year, with a relative minimum between August and October. Thunderstorms are possible throughout the year; in summer, they are generally short-lived, while in spring, they can be intense, and accompanied with wind gusts.

In Atlanta, Georgia, the slightly higher altitude, about 300 meters (1,000 feet), temper a little the summer heat: the average temperature ranges from 7 °C (44.5 °F) in January to 26.8 °C (80 °F) in July. The rains are abundant here as well, amounting to 1,280 mm (50.5 in) per year, and are well distributed throughout the year.

Subtropical climate

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In this region comprising the area bordering the Gulf of Mexico, the climate is sub-tropical, and it's warm and humid for many months of the year.
Winter is very mild, since the averages in January are higher than 9 °C (48 °F). But even here, in spite of the southern location, cold spells in winter can sometimes occur, though quite rarely; the southern part of Florida is the most sheltered and is almost always spared from the cold, to the point of having an almost tropical climate.
Here too, the western part is less humid: precipitation drops below 1,000 mm (40 in) only in south-western Texas, while starting from eastern Texas, this whole band is rainy and with plenty of thunderstorms.
The amount of sunshine is not exceptional, in fact, in the long summer season, although the sun still prevails, clouds can form in the afternoon, and can cause thunderstorms, while some tropical low pressure systems can also pass over the area.
In this area, in the month of October, and sometimes November, there's a relative lull in precipitation, with calm and pleasant days (if it is not affected by the last hurricanes of the season).

In Austin and San Antonio (Texas), the weather in winter is usually very mild, but with possible short cold waves: however, the average in January is around 10 °C (50 °F), and in the rest of the year, the temperature is similar to that of Dallas, with an equally very hot and humid summer, while tornadoes in spring are less frequent because of the greater proximity to the sea.

In the south-western tip of Texas, from Corpus Christi to the Mexican border, the winter is very mild, since highs are around 20 °C (68 °F) even in January, and the rainfall is not abundant, since it hovers between 500 and 800 mm (20 and 30 in) per year.

Houston is located about 50 kilometers (30 miles) away from the sea (but Galveston Bay borders the southeastern districts of the city): here, the average temperature ranges from 12 °C (53.5 °F) in January to 29.5 °C (85 °F) in July, when highs are around 35 °C (95 °F) and the humidity is high. It's no surprise that a city so uncomfortably hot has been the first in the world to see a widespread distribution of air conditioners.
Rainfall amounts to 1,315 mm (52 in) per year, so it's fairly abundant, and well distributed throughout the year.

In New Orleans, Louisiana, the summer temperatures are similar to those of Houston, but the omnipresence of water makes the heat even more sweltering. The rains are definitely abundant: up to 1,610 mm (63 in) per year.
Near New Orleans, the Gulf of Mexico is warm enough for swimming from May to November, and it gets very warm in the summer months. In winter, it is a bit cold, since it drops to 18 °C (64 °F).

In peninsular Florida, winter is even milder, and spring-like.
In Orlando and Tampa, the January average is around 16 °C (61 °F). There are tropical weather conditions from mid-May to September, with heat, humidity and frequent thunderstorms. April and October are hot but a little drier.

Tropical climate

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However, it's the southern part of Florida, which is a true winter refuge for many American snowbirds. Starting from the Cape Coral - Palm Beach line, the temperature in the coldest month exceeds 18 °C (64.5 °F), therefore we can speak of tropical climate.

In Miami, on the southern tip of the state and near the Tropic of Cancer, the January average is 20 °C (68 °F), so here there is no winter: the sun often shines, the air is pleasantly warm, and a nice breeze blows from the sea.
However, here too the summer is hot and muggy, sunny but with frequent thunderstorms.

Hurricanes

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The states on the Gulf of Mexico (Texas, Louisiana, Mississippi, Alabama, and Florida) as well as the southernmost Atlantic states (Georgia, North and South Carolina) can be affected by tropical depressions and hurricanes, which occasionally can also affect other Atlantic coastal states.
The areas most at risk are the coastal ones, however, hurricanes can also penetrate inland, even though, in these cases, they tend to weaken.
The hurricane season runs from June to November, although they are most likely from August to October.

Tornadoes

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Another danger comes from tornadoes, which are large and intense whirlwinds. Tornadoes are very rare in the western part of the United States (the states of the Pacific, the Rocky Mountains and the deserts) and are typical of the central and eastern states, except the northern portions of the states of the Great Lakes and of the northeast.
However, tornadoes are more frequent in the central-southern states, except on the coasts. They develop mainly along two lines: the "Tornado Alley", from South Dakota to northern Texas (north/south direction), and the "Dixie Alley", from Oklahoma to Ohio (south-west/north-east direction).
The months when they are most frequent are May and June, but they may also occur between February and April, especially in the south, while in summer, they can occur in the northern part of the Great Plains.
In Florida, tornadoes are quite frequent, but they are generally less intense than on the mainland.

When to go

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It is hard to find a single period in which the weather is the best throughout the country. In general, however, since the climate of most of the United States is cold in winter and hot in summer, you can choose spring and autumn. It must be said, however, that during spring, tornadoes are possible in the inland areas of the central and eastern part, and in autumn, hurricanes can affect the southernmost area, still of the center-east.

Being that it's mild even in summer, you can visit the west coast, including Seattle and San Francisco, from May to September.
On the coast of Southern California and in Los Angeles, you can go throughout the year, but they are preferable in spring, from March to May; in this way, you can move to the interior without fear of the heat (but in the desert, the month of May can be already hot), or to the parks of the Sierra Nevada without fear of the winter cold.
You can visit the Death Valley from November to March, however, the best months are February and March (in this way, you can reduce the risk of the cold at night). This period is generally recommended for the hot desert areas.
You can visit the Grand Canyon, in April and October, in order to avoid both the summer heat in the lower part and the winter cold of the upper part. In the high mountain areas of the Rockies, including the Yellowstone National Park, you can go in summer, from June to August.
The best periods in New York are the month of May and from mid-September to mid-October; the latter is generally a mild and relatively calm period. In winter, there's the risk of freezing cold and snow storms. In summer, there can sometimes be uncomfortable heat, while thunderstorms can break out in the afternoon. In early spring, the weather can be unstable, and sometimes cold.
This period of early autumn is good throughout the north and north-east, but also in the highlands of the western area, bearing in mind that it can already get cold at night. May is also a good month in these areas.
You can visit Miami, the Everglades and Southern Florida from November to April, but for a beach holiday, you can choose the period mid-March to late April, in order to avoid the risk of the rare but not impossible cold periods.
March-April and October-November are good periods to visit the southern regions and those bordering the Gulf of Mexico. In the former, however, tornadoes are possible away from the coast, while in the latter, especially in October, hurricanes are still possible. In winter, the weather is often pleasant, but we cannot exclude short cold waves.

What to pack

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In winter: in the northern and mountainous areas, pack cold weather clothing, such as synthetic, thermal and long underwear, a down filled parka with insulated hood, gloves, warm boots, and a benie; T-shirts and light shirts for hot indoor environments.
In New York, pack a down jacket, gloves, a scarf, and a hat.
In the Seattle area and the north-west coast, pack warm clothes, a winter coat, and a raincoat or umbrella.
In Los Angeles and Miami, pack clothes for spring and autumn, an umbrella.
In the southern states and northern Florida, clothes for spring and autumn, but also warm clothes and a warm jacket for any short cold spells.

In summer: in the northernmost areas, pack light clothing, T-shirts for hot days, a jacket and sweatshirt for the evening and for cool days, and a raincoat or umbrella.
On the west coast, down to San Francisco, pack clothes for spring and autumn: a T-shirt, a shirt, a jacket, and a sweatshirt or sweater.
In New York, Chicago, Boston and Washington: pack light clothing, a T-shirt, a jacket and a sweater for the evening and for cool days, an umbrella, a sweatshirt and a pashmina for airconditioned places.
In desert areas and the south: lightweight, loose-fitting clothing, a sun hat, a sweatshirt and a pashmina for airconditioned places, comfortable and breathable shoes; in Florida and the southern states, an umbrella or lightweight rain gear; in the deserts, a light scarf for the wind full of dust.
In the mountainous national parks: hiking shoes, a jacket and a sweatshirt or sweater for the evening, sunscreen, sunglasses, hiking boots, and a raincoat or umbrella.

Other resources available for the climate of the United States and of overseas possessions:

American Samoa (Oceania)
Hawaii (Oceania)
Puerto Rico (Caribbean)
United States Virgin Islands (Caribbean)

Climate data - United States

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See also the temperatures month by month

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