Maui Temperature

Meteorological data for Maui, Hawaii (United States)

Explanation of the graphic: Temperature range Mean temperature (24h) per mont. Temperature standards are taken over the 1961-1990 years. This chart shows the mean number of rainy 24 hours per year. If the rainfall has exceeded 1mm per 24 hours per working hour, it is considered as a rainfall per die.

Average time frame is 1961-1990.

Maui climate

Maui' s climate: Hawaii has a perfect weather every single of the year - it's hot summers in Hawaii all year round! Maui' s weather is a great attraction for Maui' s visitors, with temperate weather, low precipitation and generally sunshine in the leewards of Lahaina, Kaanapali, Kihei and Wailea.

Located in the Pacific Ocean, the Hawaii Islands are located far western and southern of the United States, but just off the northern shore of the Pacific Ocean, 1,300 to 1,500 nautical mile (? 19 to 22 latitudes, similar to Cuba in the Caribbean). Because of its mild weather, Hawaii is known as a "tropical paradise" because it is a place where every single year is a pleasure.

Hawaii's combinations of sun, temperature, air moisture and wind varies within the bounds of what is humanly comfy. Hawaii's perfect climate is between 70-82 F and 50% air moisture. When it is five° C colder than in summers, the humankind's bodies adapt somewhat to the different season.

Hawaii is on average six degree colder than summers, making Hawaii just as pleasant in both winters and summers. Hawaii really is a semi-tropical heaven, unlike many other isles that are mistakenly called "tropical paradise", where it felt quite unpleasant at very warm 1990s and humid 1990s soils.

This makes the year round Clubmate in Howaii the best. HAWAIlI WHEATHER can sometimes change, especially in the case of stormy winters. The five-month tourist seasons (May to September) have the best hot sea conditions and very few windstorms. In the Maui summers the temperature is ideally in the shadow; and in the early mornings & later afternoons and at nights in the south.

The seven-month wintersason ( "October to April") is perfect in the arid areas of Lahaina and Wailea (which can be a bit too warm in summer). In the Maui winters, the daytime temperature is perfect in the sun, but the beach can sometimes be a bit too cold and drab or rain.

One of the most prominent features of the Hawaiian temperature is the small yearly temperature area. The hottest time of August in Honolulu's city centre is the coolest one, with an mean temperature of around 78° Celsius, and around 72 Celsius in February - the area between the hottest and coolest of the year is only 6 Celsius on averaging.

The reason for this is in part the almost steady current of sea breezes over the island, especially with the Hawaiian situation in the middle of the sea. Sea temperatures vary relatively little from one seasons to the next, as does the temperature of the sea breeze, which has travelled across the oceans for long periods of time.

This is how the warm temperature typical of the sea around us is brought to the hawaiian isles. Open oceans around the island of Manhattan have an mean temperature ranging from a least 73 or 74 degrees Fahrenheit between the end of February and early April to a peak of 79 or 80 degrees Fahrenheit at the end of September or early October.

At almost as balmy a temperature of several hundred kilometres, even in the northern hemisphere, the skies reaching Hawaii are neither very warm nor soaring. During the low 1990s, the temperature in the arid leewards such as Lahaina and Wailea can reach several times a year on several nights, but higher temperature is uncommon.

These arid areas, like the rest of Hawaii, are the hottest in August and September. In the 1950s, the lower levels were recorded in winters at altitudes below 1,000 ft or in the high 1940s in arid leewards. This is an extremum and it is possible that several years may elapse before the temperature reaches 50 degrees Celsius at any point near the surface of the world.

The leewards of Kaanapali and Wailea, well protected from the the tradewinds and along the western coast of Maui, have between 30 and 60 per cent of the clear light and less than 20 per cent of the clouds. The leewards, which are less affected by the Passat cloud in spring, are rather overcast in the cold season, when the storm is more common.

Most of the precipitation in summers is due to passat wind, and these rainfall is most likely to take place at midnight. Most of the precipitation in the plains in winters takes the form of storm, which can strike both during the day and at nights. Precipitation varies greatly from year to year in most parts of the tropical region, and Hawaii is no different.

Precipitation versatility is much greater in winters, when sporadic windstorms make a significant contribution to precipitation, than in summers, when the majority of precipitation comes from trans-Passta. The Passat breeze lowers the seeming temperature on warm weather which makes the weather much more comfortable than the temperature and air damp. For example, in the case of moderately windy trades, less than half a per cent of the period occurs at an air moisture level of up to 70 per cent.

August, September, October and November are the only few moths in which the temperature exceeds one per cent of the year. From May to September, the trade wind blows 80 to 95 per cent of the air over Hawaii. Between October and April, when the wind is blowing through Hawaii, the trading still blows 50 to 80 per cent of the year.

Averages are highest during the Hawaiian sea's daylight passat season. Windspeeds over the oceans top 50 per cent of the clock during the summers (May to September). Eighty-95 per cent of the times these storms come from the Northeastern-Quadrants.

Winters are the period of occasionally very heavy wind - higher than in summers (with the exception of the uncommon appearance of a tropic windstorm or cyclone in summer). If the wind is calm and flexible, the humid climate can move gradually to the island, usually from the southeastern, southern or southwestern regions.

It is a vulcanic smoulder from the Big Island vulcano in the southern hemisphere, which moves northwards to Maui on a regular basis when the north-east tram stop blower. Sometimes the floating minute particulates are so thick that they erase the view of Lanai and Molokai of Maui and also keep them in the heats of the day, which leads to warm weather on Maui and possible trouble for anyone with respiratory illness.

Hawaiian waters are perfect for swim, with an mean temperature of at least 73 or 74 degrees Celsius between the end of February and early April to a peak of 79 or 80 degrees Celsius at the end of September or early October. Summers are the time of year when the direct or almost direct sunlight is above us, the climate is warm and the trade wind is the most dependable.

There is a five-month long holiday period (May to September). Summers are definitely the warmest, the most prevalent time of year for trades-wins, and the time of year when rains are not common. Summers are also the driest time of the year, measured by mean precipitation per month. Winters are the time of year when the southern hemisphere is sunny, the climate is colder and the Tradewind is usually disturbed by other wind.

There is a seven-month long winterseason ("October to April"). Great winds are mainly occurrences of the wintry time. Larger windstorms are most frequent between October and March. There can be two, three or even up to six or seven big windstorms in a certain year.

These types of windstorms usually cause strong rainfall, sometimes with very strong currents from all directions. The resulting windspeeds have surpassed 60 MPH several times over a one to two minute span, and 80 MPH briefly in gusty conditions. Windstorms, large or small, usually arise during a collapse of the north east' side of the Passat.

Cona Storm occurs during the cold seasons. They' re so named because they often carry southern breezes (called cona in Hawaiian), as opposed to the common northeastern Tradewindstorm. Today, the concept is used more and more by the locals when there is a common rain shower, flanked by breezes from a different area.

The Kona Tempest brings rains to the most protected and arid, south-facing areas of Lahaina and Wailea. Precipitation in a Kona gale is more common and longer than in the normal Kaltfront sturm - but not as severe as in the more severe wind of the Kaltfrontstürme.

Normally there are one or two Kona gales a year, and sometimes there are four or five. Though a whole winters can go by without a Kona thunderstorm. The Kona Rain lasts from several hrs to several day. Maui' s year round climates are excellent, but the local conditions vary. The two high peaks of Maui protect the western and southern shores from the northeastern cold winds, leading to almost flawless conditions in the Kaanapali and Wailea area.

There, the climate is arid, with the exception of occasionally slight passat shower, which drifts over the hills from upwind. In Maui you will almost always find a place in the sun - because the hills are blocking the cloud and the rains. In Maui, it says: "If you don't like the climate, just go five mile!

" When it is rainy and breezy at your Kapalua resort (where it often rain in winter), you can travel four kilometres to Kaanapali where it is usually sun-sound. However, when it is overcast there, you can continue four kilometres further southwards to the city of Lahaina, where it is almost every single morning of the year mild and sunshine because the hill protects it from storm.

West Maui is located at the foot of the West Maui Mountains, which are 5,000 ft high, high enough to freeze most storm events and cause the West Maui Microclimates. The South Maui Resort is located at the foot of Haleakala Hill, which is 10,000 ft high, high and solid enough to stop practically all winds.

When it rains and winds at your Kihei resort, you can travel four kilometres to Wailea four kilometres southwards, and when it is not rainy but overcast, you can travel four more kilometres southwards to the Makena area, where it is sunshine and tranquillity almost every year.

Maui' s most conspicuous meteorological contrast is the amount of precipitation. SMALL RAIN - Some areas have an annual mean of 20in and less, in the southern and west Leeküstengebieten behind the two very high hills, at an extrem. From October to May, great winds can leave one footed or more snows on the top of Maui' s highest peak, Haleakala.

However, the snows disappear quickly, as even the temperature in Hawaii is usually above zero in cold time. Real cyclones are very uncommon in Hawaii, as shown by the fact that only four of them have hit the island over a 63-year peril. However, storms can go near enough to the island to generate strong rainfall, strong wind and large coastal swell.

There are more tropic gales. They are similar to a hurricane, but with more moderate wind speeds, below 74 MPH. Each year, on an annual basis, a hurricane passes by near Hawaii to influence the climate in some parts of the islands. In contrast to the Kaltfront and Kona gales, cyclones and tropics are not restricted to the conservative seasons.

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