Sluice Point in Nova Scotia
Sluice Point (French : Pointe du Sault) is a community in the Canadian province of Nova Scotia, located in the Argyle Municipality in Yarmouth County.
Sluice Point (French : Pointe du Sault) is a community in the Canadian province of Nova Scotia, located in the Argyle Municipality in Yarmouth County.
The school started with the primary department in 1870. There was opposition to both the school and the Indian Sluice Point Bridge (to Surette's Island). Education was not well understood then, and one man, Jacques Babin, stubbornly affirmed that no bridge or school would be built while he was alive. In the primary department there were about twenty-five seats. It was big enough at that time, but the population increased, so they built the advanced department in 1902. [1]
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Sluice Point lies on a climatic zone known as a humid continental climate (Köppen climate classification Dfb). [3] Winters are cool and snowy or rainy with a January average of −4.3 °C (24.3 °F), temperatures below −20 °C (−4.0 °F) are rare for the area, and the average high never drops to below freezing at any point in the year. [2] During this period of time, the weather can be unsettled and cloudy due to the Nor'easters coming up the coast from the southwest, however in the past few years there has been an absence of snowfall. [4] As a result, Sluice Point averages only 85–170 hours of sunshine from December to February or 36%–44% of possible sunshine. [2] The average annual snowfall is 207 centimetres (81 in), which can come from Nor'easters from the southwest with a maximum snow depth of 7 centimetres (3 in) in January, owing to its mild winters, among the mildest in Canada east of the Rockies. [4]
Sluice Point's summers are warm due to the woodlands which keeps summer temperatures warm, meaning temperatures above 25 °C (77.0 °F) are common. [4] The average high temperature in the warmest month, August is 27.9 °C (82.2 °F). Spring and fall are transitional seasons in which falls are warmer than spring since the waters are at the warmest temperatures in fall and the coldest during early spring. [4] July and August the driest months on average and November the wettest month on average.
The highest temperature ever recorded in Sluice Point was 36.3 °C (97.3 °F) on 2 August 2016. [5]
The United Kingdom straddles the higher mid-latitudes between 49° and 61°N on the western seaboard of Europe. Since the UK is always in or close to the path of the polar front jet stream, frequent changes in pressure and unsettled weather are typical. Many types of weather can be experienced in a single day.
Yarmouth is a port town located on the Bay of Fundy in southwestern Nova Scotia, Canada. Yarmouth is the shire town of Yarmouth County and is the largest population centre in the region.
A Mediterranean climate, also called a dry summer climate, described by Köppen as Cs, is a temperate climate type that occurs in the lower mid-latitudes. Such climates typically have dry summers and wet winters, with summer conditions being hot and winter conditions typically being mild. These weather conditions are typically experienced in the majority of Mediterranean-climate regions and countries, but remain highly dependent on proximity to the ocean, altitude and geographical location.
An oceanic climate, also known as a marine climate or maritime climate, is the temperate climate sub-type in Köppen classification represented as Cfb, typical of west coasts in higher middle latitudes of continents, generally featuring cool to warm summers and cool to mild winters, with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 40 and 60 degrees latitude, with subpolar versions extending to 70 degrees latitude in some coastal areas. Other varieties of climates usually classified together with these include subtropical highland climates, represented as Cwb or Cfb, and subpolar oceanic or cold subtropical highland climates, represented as Cfc or Cwc. Subtropical highland climates occur in some mountainous parts of the subtropics or tropics, some of which have monsoon influence, while their cold variants and subpolar oceanic climates occur near polar or tundra regions.
The climate of Salt Lake City, Utah features cold and snowy winters, hot and dry summers, and modest to light seasonal rainfall. Lying in the Salt Lake Valley, the city is surrounded by mountains and the Great Salt Lake. Under the Köppen climate classification, Salt Lake City has either a Mediterranean climate (Csa) or dry-summer continental climate (Dsa) depending on which variant of the system is used, though it borders on a cold semi-arid climate (BSk) due to the city's relatively low precipitation.
The climate of Bismarck in the U.S. state of North Dakota is humid continental, caused primarily by the combination of its mid-level latitude and location not far from the geographic centre of the U.S. Its summers are hot enough for it to border on having a Köppen Dwa classification, and precipitation is high enough for it to barely avoid being classified as semi-arid. The city's climate displays four very distinct seasons and great variation in temperatures over very short periods of time. Like other cities in the northern Great Plains, its climate is also fairly dry.
Yarmouth, officially named the Municipality of the District of Yarmouth, is a district municipality in Yarmouth County, Nova Scotia, Canada. Statistics Canada classifies the district municipality as a municipal district.
Ingonish is a popular tourist destination in Victoria County, Cape Breton Island, Nova Scotia, Canada. The regional economy is tied to fishing and tourism. Tourist facilities include Cape Breton Highlands National Park, the Keltic Lodge, a downhill skiing centre, and a public golf course, the Highlands Links.
Columbus, Ohio has a humid continental climate, characterized by humid, hot summers and cold winters, with no dry season. The Dfa climate has average temperatures above 22 °C during the warmest months, with at least four months averaging above 10 °C, and below 0 °C during the coldest. The climate is transitional with the Cfa humid subtropical climate to the south, characterized by humid, hot summers and cool winters.
The climate of the United States varies due to changes in latitude, and a range of geographic features, including mountains and deserts. Generally, on the mainland, the climate of the U.S. becomes warmer the farther south one travels, and drier the farther west, until one reaches the West Coast.
Most regions of Japan, such as Honshu, Shikoku, and Kyushu, belong to the temperate zone with humid subtropical climate characterized by four distinct seasons. However, its climate varies from cold humid continental climate in the north such as northern Hokkaido, to warm tropical rainforest climate in the south such as the Yaeyama Islands and Minami-Tori-shima.
The climate of Ireland is mild, humid and changeable with abundant rainfall and a lack of temperature extremes. Ireland's climate is defined as a temperate oceanic climate, or Cfb on the Köppen climate classification system, a classification it shares with most of northwest Europe. The island receives generally warm summers and cool winters.
The climate of Finland is influenced most by its latitude: Finland is located between 60 and 70 N. Because of Finland's northern location, winter is the longest season. Only on the south coast and in the southwest is summer as long as winter. On average, winter lasts from early January to late February in the outermost islands in the archipelago and the warmest locations along the southwestern coast – notably in Hanko – and from early October to mid May in the most elevated locations, such as northwestern Lapland and the lowest valleys in northeastern Lapland. This means that southern portions of the country are snow-covered about three to four months of the year, and the northern for about seven months. The long winter causes about half of the annual 500 to 600 millimetres precipitation in the north to fall as snow. Precipitation in the south amounts to about 600 to 700 millimetres annually. Like that of the north, it occurs all through the year, though not so much of it is snow.
Malta has a Subtropical-Mediterranean climate according to the Köppen climate classification (Csa), with very mild winters and warm to hot summers. Rain occurs mainly in winter, with summer being generally dry. According to the Troll-Paffen climate classification and the Siegmund/Frankenberg climate classification, Malta lies within the subtropical zone, being at 35ºN latitude.
A humid subtropical climate is a temperate climate type characterized by hot and humid summers, and cool to mild winters. These climates normally lie on the southeast side of all continents, generally between latitudes 25° and 40° and are located poleward from adjacent tropical climates, and equatorward from either humid continental or oceanic climates. It is also known as warm temperate climate in some climate classifications.
Milton Highlands is a designated place located 2 km (1.2 mi) from the town of Yarmouth within the Municipality of the District of Yarmouth in Nova Scotia, Canada.
Estonia lies in the northern part of the temperate climate zone and in the transition zone between maritime and continental climate. Because Estonia is continuously warmed by maritime air influenced by the heat content of the northern Atlantic Ocean, it has a milder climate despite its northern latitude. The Baltic Sea causes differences between the climate of coastal and inland areas.
The climate of Allentown, Pennsylvania is classified as a humid continental climate. Allentown's warmest month is July with a daily average temperature of 74.7 °F (23.7 °C) and the coldest month being January with a daily average of 29.4 °F (−1.4 °C). The average precipitation of Allentown is 45.35 inches (1,152 mm) per year.
Barcelona has a Mediterranean climate (Csa) according to Köppen-Geiger classification, a warm-temperate subtropical climate according to Troll-Paffen climate classification, and a subtropical climate according to Siegmund/Frankenberg climate classification.
Nova Scotia lies in the mid-temperate zone, and although the province is almost surrounded by water, the climate is closer to continental climate rather than maritime climate. The temperature extremes of the continental climate are moderated by the ocean.