Tatlayoko Lake, British Columbia

Last updated

Tatlayoko Lake
Canada British Columbia location map 2.svg
Red pog.svg
Tatlayoko Lake
Location of Tatlayoko Lake in British Columbia
Canada location map 2.svg
Red pog.svg
Tatlayoko Lake
Tatlayoko Lake (Canada)
Coordinates: 51°39′54″N124°24′06″W / 51.66500°N 124.40167°W / 51.66500; -124.40167
CountryCanada
Province British Columbia

Tatlayoko Lake is an unincorporated settlement and locality on the Homathko River just north of that river's entry into the lake of same name, [1] which is located in the western Chilcotin Country of the Central Interior of British Columbia, Canada.

Contents

Climate

The name Tatlayoko is derived from the Tsilhqot'in language and means "lake of the big winds." [2] True to its name, the community is windy throughout the fall and winter as the warm Chinook winds blow up the valley. The Chilcotin Plateau is known for being extremely cold in the winter, but Tatlayoko Lake is an exception thanks to its proximity to the mild Pacific Ocean. While the coastal winds bring the community relatively mild winters, the mountains block most of the coastal precipitation, leaving the community comparatively dry.

In relation to the nearby community of Tatla Lake and indeed the rest of the Chilcotin Plateau off to the east, Tatlayoko Lake tends to be wetter in the winter and drier in the summer. Tatlayoko Lake has a continental climate (Dfb), bordering on a subarctic climate (Dfc).

The hottest temperature on record on June 29, 2021 when the temperature climbed to 39.6 °C (103 °F).

Weather facts

Climate data for Tatlayoko Lake
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Record high °C (°F)15.6
(60.1)
17.8
(64.0)
21.4
(70.5)
29.4
(84.9)
33.5
(92.3)
39.6
(103.3)
37.8
(100.0)
33.9
(93.0)
32.2
(90.0)
27.8
(82.0)
18.3
(64.9)
15
(59)
37.8
(100.0)
Mean daily maximum °C (°F)−0.7
(30.7)
3.0
(37.4)
7.2
(45.0)
11.8
(53.2)
16.1
(61.0)
19.3
(66.7)
22.4
(72.3)
22.7
(72.9)
18.6
(65.5)
11.5
(52.7)
3.1
(37.6)
−1.6
(29.1)
11.1
(52.0)
Daily mean °C (°F)−5.7
(21.7)
−2.9
(26.8)
0.7
(33.3)
4.5
(40.1)
8.3
(46.9)
11.6
(52.9)
13.9
(57.0)
13.9
(57.0)
10.1
(50.2)
4.8
(40.6)
−1.6
(29.1)
−6.3
(20.7)
4.3
(39.7)
Mean daily minimum °C (°F)−10.5
(13.1)
−8.7
(16.3)
−5.7
(21.7)
−2.8
(27.0)
0.6
(33.1)
3.7
(38.7)
5.4
(41.7)
5.0
(41.0)
1.5
(34.7)
−1.8
(28.8)
−6.2
(20.8)
−11.1
(12.0)
−2.6
(27.3)
Record low °C (°F)−43.3
(−45.9)
−37.2
(−35.0)
−32.8
(−27.0)
−21.1
(−6.0)
−10
(14)
−5
(23)
−3
(27)
−4
(25)
−9.5
(14.9)
−27
(−17)
−39
(−38)
−40.6
(−41.1)
−43.3
(−45.9)
Record low wind chill −45−37−36−20−13−6−5−5−11−22−41−39−45
Average precipitation mm (inches)42.2
(1.66)
23.2
(0.91)
26.7
(1.05)
20.0
(0.79)
31.9
(1.26)
37.3
(1.47)
39.6
(1.56)
33.8
(1.33)
26.9
(1.06)
53.7
(2.11)
55.3
(2.18)
47.0
(1.85)
435.5
(17.15)
Average rainfall mm (inches)20.2
(0.80)
9.9
(0.39)
14.6
(0.57)
15.0
(0.59)
29.8
(1.17)
37.3
(1.47)
39.6
(1.56)
33.8
(1.33)
26.5
(1.04)
50.2
(1.98)
31.5
(1.24)
16.7
(0.66)
324.7
(12.78)
Average snowfall cm (inches)20.0
(7.9)
13.4
(5.3)
12.1
(4.8)
5.0
(2.0)
2.1
(0.8)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.4
(0.2)
3.5
(1.4)
23.8
(9.4)
30.7
(12.1)
110.8
(43.6)
Average relative humidity (%)70.055.053.138.643.846.137.334.636.847.470.773.050.5
Source: Environment Canada [3]

Related Research Articles

<span class="mw-page-title-main">Subarctic climate</span> Climate characterised by long, usually very cold winters, and short, cool summers

The subarctic climate is a continental climate with long, cold winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, generally at latitudes from 50°N to 70°N, poleward of the humid continental climates. Subarctic or boreal climates are the source regions for the cold air that affects temperate latitudes to the south in winter. These climates represent Köppen climate classification Dfc, Dwc, Dsc, Dfd, Dwd and Dsd.

<span class="mw-page-title-main">Williams Lake, British Columbia</span> City in British Columbia, Canada

Williams Lake is a city in the Central Interior of British Columbia, in the central part of a region known as the Cariboo. Williams Lake is one of the largest cites, by population of metropolitan area, in the Cariboo after neighbouring Quesnel. The city is famous for the Williams Lake Stampede, which was once the second largest professional rodeo in Canada, after only the Calgary Stampede.

<span class="mw-page-title-main">Gold River, British Columbia</span> Village in British Columbia, Canada

Gold River is a village municipality located close to the geographic centre of Vancouver Island in British Columbia, Canada. In terms of the Island's human geography it is considered to be part of the "North Island", even though it technically is on the Island's west coast.

<span class="mw-page-title-main">Mesopotamia, Argentina</span> Region in Argentina

La Mesopotamia or Región Mesopotámica is the humid and verdant area of northeast Argentina, comprising the provinces of Misiones, Entre Ríos, and Corrientes. The landscape and its characteristics are dominated by two rivers: the Paraná and the Uruguay.

The Chilcotin region of British Columbia is usually known simply as "the Chilcotin", and also in speech commonly as "the Chilcotin Country" or simply Chilcotin. It is a plateau and mountain region in British Columbia on the inland lee of the Coast Mountains on the west side of the Fraser River. Chilcotin is also the name of the river draining that region. In the language of the Tsilhqot'in people, their name and the name of the river means "those of the red ochre river". The proper name of the Chilcotin Country, or Tsilhqotʼin territory, in their language is Tŝilhqotʼin Nen.

<span class="mw-page-title-main">Chilcotin River</span> River in southern British Columbia, Canada

The Chilcotin River /tʃɪlˈkoʊtɪn/ located in Southern British Columbia, Canada is a 241 km (150 mi) long tributary of the Fraser River. The name Chilcotin comes from Tŝilhqot’in, meaning "ochre river people," where ochre refers to the mineral used by Tŝilhqot’in Nation and other Indigenous communities as a base for paint or dye. The Chilcotin River, Chilko River and Lake, and Taseko River and Lake make up the Chilcotin River watershed. This 19,200 km2 (7,400 sq mi) watershed drains the Chilcotin Plateau which reaches north to south from the Nechako Plateau to Bridge River county and east to west from Fraser River to the Coast Mountains. It is also one of twelve watersheds that make up the Fraser River Basin. Made up of seven major tributaries, Chilcotin River starts northeast of Itcha Mountain, flowing southeast until it joins the Fraser River south of Williams Lake, 22 km (14 mi) upstream from Gang Ranch.

<span class="mw-page-title-main">Bella Coola, British Columbia</span> Town in British Columbia, Canada

Bella Coola is a unincorporated community in the Bella Coola Valley of British Columbia, Canada. Bella Coola usually refers to the entire valley, encompassing the settlements of Bella Coola proper, Lower Bella Coola, Hagensborg, Salloompt, Nusatsum, Firvale, and Stuie. It is also the location of the head offices of the Central Coast Regional District.

<span class="mw-page-title-main">Geography of British Columbia</span>

British Columbia is the westernmost province of Canada, bordered by the Pacific Ocean. With an area of 944,735 km2 (364,764 sq mi) it is Canada's third-largest province. The province is almost four times the size of the United Kingdom and larger than every United States state except Alaska. It is bounded on the northwest by the U.S. state of Alaska, directly north by Yukon and the Northwest Territories, on the east by Alberta, and on the south by the U.S. states of Washington, Idaho, and Montana. Formerly part of the British Empire, the southern border of British Columbia was established by the 1846 Oregon Treaty. The province is dominated by mountain ranges, among them the Canadian Rockies but dominantly the Coast Mountains, Cassiar Mountains, and the Columbia Mountains. Most of the population is concentrated on the Pacific coast, notably in the area of Vancouver, located on the southwestern tip of the mainland, which is known as the Lower Mainland. It is the most mountainous province of Canada.

<span class="mw-page-title-main">Homathko River</span> River in British Columbia, Canada

The Homathko River is one of the major rivers of the southern Coast Mountains of the Canadian province of British Columbia. It is one of the few rivers that penetrates the range from the interior Chilcotin Country to the coastal inlets of the Pacific Ocean. The Homathko River reaches the sea at the head of Bute Inlet, just west of the mouth of the Southgate River.

<span class="mw-page-title-main">Geography of Toronto</span> Geography of the city of Toronto, Canada

The geography of Toronto, Ontario, covers an area of 630 km2 (240 sq mi) and is bounded by Lake Ontario to the south; Etobicoke Creek, Eglinton Avenue, and Highway 427 to the west; Steeles Avenue to the north; and the Rouge River and the Scarborough–Pickering Townline to the east. In addition to Etobicoke Creek and the Rouge River, the city is trisected by two minor rivers and their tributaries, the Humber River in the west end and the Don River east of downtown. Both flow southward to Lake Ontario at Humber Bay and Toronto Harbour respectively, which are part of the longer Waterfront, as well as Etobicoke Creek and the Rouge River.

The Taseko River or Dasiqox in the original Chilcotin, is a tributary of British Columbia's Chilko River, a tributary of the Chilcotin River which joins the Fraser near the city of Williams Lake.

<span class="mw-page-title-main">Climate of Alaska</span> Overview of the climate of the U.S. state of Alaska

The climate of Alaska is determined by average temperatures and precipitation received statewide over many years. The extratropical storm track runs along the Aleutian Island chain, across the Alaska Peninsula, and along the coastal area of the Gulf of Alaska which exposes these parts of the state to a large majority of the storms crossing the North Pacific. The climate in Juneau and the southeast panhandle is a mid-latitude oceanic climate, in the southern sections and a subarctic oceanic climate in the northern parts. The climate in Southcentral Alaska is a subarctic climate due to its short, cool summers. The climate of the interior of Alaska is best described as extreme and is the best example of a true subarctic climate, as the highest and lowest recorded temperatures in Alaska have both occurred in the interior. The climate in the extreme north of Alaska is an Arctic climate with long, cold winters, and cool summers where snow is possible year-round.

<span class="mw-page-title-main">Climate of Texas</span> Overview of the climate of the U.S. state of Texas

Texas' weather varies widely, from arid in the west to humid in the east. The huge expanse of Texas encompasses several regions with distinctly different climates: Northern Plains, Trans-Pecos Region, Texas Hill Country, Piney Woods, and South Texas. Generally speaking, the part of Texas that lies to the east of Interstate 35 is subtropical, while the portion that lies to the west of Interstate 35 is arid desert.

<span class="mw-page-title-main">Climate of South Africa</span>

The climate of South Africa is determined by South Africa's situation between 22°S and 35°S, in the Southern Hemisphere's subtropical zone, and its location between two oceans, Atlantic and the Indian.

Tatla Lake is a small unincorporated community in the west Chilcotin area of British Columbia, Canada, located at the west end of its eponymous lake. Situated 220 km west of Williams Lake along Highway 20, Tatla Lake's 123 people live approximately halfway between the two ends of the highway; Williams Lake to the east and the coastal community of Bella Coola to the west. The community is the service centre for three major mountain valleys of West Branch, Chilko and Tatlayoko. These valleys extend southward via secondary roads.

<span class="mw-page-title-main">Climate of Tasmania</span>

Tasmania has a cool temperate climate with four distinct seasons. The highest recorded maximum temperature in Tasmania is 42.2 °C (108.0 °F) at Scamander on 30 January 2009, during the 2009 southeastern Australia heat wave. Tasmania's lowest recorded minimum temperature is −14.2 °C (6.4 °F) on 7 August 2020, at Central Plateau.

<span class="mw-page-title-main">Climate of Vietnam</span> Characteristics of the climate of Vietnam

Vietnam has a monsoon-influenced climate typical of that of mainland Southeast Asia. The diverse topography, long latitude, and influences from the South China Sea lead to climatic conditions varying significantly between regions. The northern region experiences a monsoonal and temperate climate (Cfa) with four distinct seasons with winters typically dry and summers ranging from hot to mild. In more southern areas, the climate is tropical monsoon (Aw) with only two seasons. In addition, a temperate climate exists in mountainous areas, which are found in Sa Pa and Da Lat, while a more continental climate exists in Lai Châu Province and Sơn La Province.

<span class="mw-page-title-main">Climate of Los Angeles</span>

The climate of Los Angeles is mild to hot year-round, and mostly dry. It is classified as a Mediterranean climate, which is a type of subtropical climate. It is characterized by seasonal changes in rainfall—with a dry summer and a winter rainy season. Under the Köppen climate classification, the coastal areas are classified as Csb, and the inland areas as Csa.

Chilanko Forks is an unincorporated settlement as well as a First Nations community of the Tsilhqot'in people, located on the north bank of the Chilanko River just northeast of Tatla Lake, and immediately south of Puntzi Lake, in the Chilcotin District of the Central Interior of British Columbia. Chilanko Forks is the location of the offices of the Alexis Creek First Nation.

The Northwestern Forested Mountains is a Level I ecoregion of North America designated by the Commission for Environmental Cooperation (CEC) in its North American Environmental Atlas.

References

    • "Tatlayoko Lake (locality)". BC Geographical Names .
  1. "Travel and Recreation in the West Chilcotin" . Retrieved 14 March 2013.
  2. Environment CanadaCanadian Climate Normals 1981–2010 Station Data, accessed 30 July 2014