User:Grant Exploit/sandbox

Scott Island Climate section and weatherbox (WIP)
For: Scott Island Scott Island has a hyperoceanic ice cap climate (Köppen climate classification EF), as registered by an automatic weather station on the island from December 1987 to March 1999. The records show an average temperature of a few °C (°F) below 0 °C in summer, and down to -40 °C in winter. Summers are cold, though the extreme influence of the ocean makes temperatures very consistent. The highest temperature ever recorded was 4.8 °C on 10 January 1989, low even by coastal Antarctic standards. The lowest temperature ever recorded was -32.2 °C on 2 August 1998, very high for Antarctica.

Green Canyon Climate section and weatherbox (WIP)
For: Green Canyon

As recorded by a station in Block 184, the air above Green Canyon has a tropical rainforest climate (Köppen climate classification Af), with warm winters and extremely oppressive summers. Diurnal temperature variation is very low year-round (especially in summer), expected for its location far from any landmasses. Experiencing the purest Gulf influences possible, Green Canyon's summer nighttime low temperatures are some of the highest on Earth for any non-arid location, at least counting those on land. Temperatures below freezing are unknown.

The hot, humid air and warm water during summer and autumn can facilitate the development and sustainment of tropical cyclones, specifically Atlantic hurricanes, the water having surface temperatures above 26 C—the typical threshold for tropical development—from May 25 to October 31 on average, and reaching a maximum of 30 C on August 5. Precipitation is relatively evenly distributed throughout the year, peaking in late summer at the height of the hurricane season, having a secondary peak in winter, and reaching its nadir in late spring.

Linares, Chile Climate section and weatherbox (WIP)
For Linares, Chile:

Linares has a mild mediterranean climate (Köppen: Csb). The summers are hot and mainly dry (November to March) with temperatures reaching up to 32 -33 degrees Celsius on the hottest days. The winters (late May to mid September) tend to be rather humid and rainy, with typical maximum daily temperatures of 14-15 degrees Celsius, and minimum just above freezing.

Corbeta Uruguay Climate section and weatherbox (WIP)
For: Corbeta Uruguay base and Climate of South Georgia and the South Sandwich Islands

Corbeta Uruguay reported weather data only on discontinuous days (see table below) from April 1979 to April 1982, and as such our understanding of the climate of Thule Island is very incomplete. The data that does exist indicates that Corbeta Uruguay has a tundra climate (Köppen ET) that is exceptionally cold for its location less than two-thirds the distance from the Equator to the South Pole, particularly in summer.

Driest, warmest Antarctic climate weatherbox (WIP)
Based on: Villa Las Estrellas (Weather box "shell"), warmest and driest monthly figures in Antarctica (Weather box data, non-glaciated areas).

Wettest, warmest Antarctic climate weatherbox (WIP)
Based on: Villa Las Estrellas (Weather box "shell"), warmest and wettest monthly figures in Antarctica (Weather box data, non-glaciated areas).

Beansfordshire weatherbox (WIP)
Based on: Template: Heathrow Airport weatherbox, but filled with correct information the Bri'ish don't want you to know.

Lake Vostok weatherbox (WIP)
Based on: Template: Vostok Station weatherbox, extrapolating from that elevation to the level of Lake Vostok with the maximum dry adiabatic lapse rate.

Deaver, Wyoming at lowest Wyoming elevation Geography (WIP)
Based on: Deaver, Wyoming, extrapolating from its elevation to the lowest found in Wyoming with the dry adiabatic lapse rate.

Deaver is located at 44.89056°N, -108.59694°W (44.890439, −108.596860).

According to the United States Census Bureau, the town has a total area of 1.01 sqmi, all land.

Deaver is located in a sheltered valley to the west of the Big Horn Mountains and has a cold desert climate (Köppen BWk), a very rare type of climate so far north in North America and due to its very shielded location from moisture-bearing winds. Winters are almost snowless despite being very cold, with a median snowfall of only 1.4 in, though as much as 12.1 in fell in April 1973. In the summer, days can be hot but humidity is low and nights are pleasantly cool. The shielded location means that the very limited rainfall of around 5.5 in is confined to late spring and early summer thunderstorms.

Cooler Death Valley weatherbox (WIP)
Based on: Synthesis of highest valid average highs and lows recorded for each month.

Hotter Death Valley weatherbox (WIP)
Based on: Synthesis of highest valid average highs and lows recorded for each month.

Taloyoak Climate in an ice-sheet-free world (WIP)
Based on: Taloyoak#Climate, modified by "Departures from Standard" in a Clima-Sim scenario where all Permanent Ice is replaced by Water/Pack Ice. Using standard record technique (with possible order retention) and vapor-pressure-based precipitation method.

Taloyoak has a Subarctic climate (Köppen Dfc) with short, mild summers and long, cold winters.

Iqaluit Geography in an ice-sheet-free world (WIP)
Based on: Iqaluit, modified by "Departures from Standard" in a Clima-Sim scenario where all Permanent Ice is replaced by Water/Pack Ice. sing standard record technique (with possible order retention) and vapor-pressure-based precipitation method.

Iqaluit is the northernmost city in Canada, at 63 degrees north of the Equator. Iqaluit is located in the Everett Mountains, which rise from Koojesse Inlet, an inlet of Frobisher Bay, on the southeast part of Baffin Island. It is well to the east of Nunavut's mainland, and northeast of Hudson Bay.

Climate
Iqaluit has a tundra climate (Köppen: ET) typical of the Arctic region, although it is well outside the Arctic Circle. The city features very long, cold winters and brief, cool summers. Average monthly temperatures are below freezing for eight months of the year. Iqaluit averages just over 400 mm of precipitation annually, much wetter than many other localities in the Arctic Archipelago, with the summer being the wettest season. Temperatures of the winter months are comparable to other northern communities further west on the continent such as Yellowknife and to some extent even Fairbanks, Alaska, even though Iqaluit is a few degrees colder than the latter. Summer temperatures are, however, much colder due to its easterly maritime position affected by the waters of the cold Baffin Island Current. This means that the tree line is much further south in the eastern part of Canada, being as southbound, in spite of low elevation, as northern Labrador.

Although it is north of the natural tree line, there are some short, south-facing imported black spruce (Picea mariana) specimens protected by snowdrifts in the winter, in addition to a few shrubs, which are woody plants. These include the Arctic willow (Salix arctica), which is hard to recognize as a tree because of its low height. The Arctic willow may be up to around 25 ft horizontally, but only 6 in tall.

The climate of Iqaluit is also colder than Gulf Stream locations on the same latitude. For example, the Norwegian city of Trondheim has an annual mean temperature that is 15.2 C-change milder.

The lowest temperature ever recorded was -45.6 C on 10 February 1967. The highest temperature ever recorded in Iqaluit was 26.7 C on 21 July 2008.

Cartwright, Newfoundland and Labrador Climate in an ice-sheet-free world (WIP)
Based on: Cartwright, Newfoundland and Labrador, modified by "Departures from Standard" in a Clima-Sim scenario where all Permanent Ice is replaced by Water/Pack Ice. Using standard record technique (with possible order retention) and vapor-pressure-based precipitation method.

Cartwright has a subarctic climate (Dfc) with very snowy winters and short, mild summers. Owing to its maritime location, the winters are however a little milder than on most of the Labrador Peninsula, but snow depth from the stormy Icelandic Low, which circulates cold and saturated air around the region, is extreme: it averages around 160 cm at its peak early in March and has reached as high as 351 cm on April 7, 2003. Snow is usually fully melted early in June and is established again in early November. Unlike most of Labrador, there is no permafrost because of the insulation from the deep snow cover, although the annual mean temperature is 0.0 C.

Essex, Ontario Climate in an ice-sheet-free world (WIP)
Based on: Essex, Ontario, modified by "Departures from Standard" in a Clima-Sim scenario where all Permanent Ice is replaced by Water/Pack Ice. Using standard record technique (with possible order retention) and vapor-pressure-based precipitation method.

Burlington, Vermont Geography in an ice-sheet-free world (WIP)
Based on: Burlington, Vermont, modified by "Departures from Standard" in a Clima-Sim scenario where all Permanent Ice is replaced by Water/Pack Ice. Using standard record technique (with possible order retention) and vapor-pressure-based precipitation method.

The city of Burlington is situated on the eastern shore of Lake Champlain, north of Shelburne Bay. It was built on a strip of land extending about 6 mi south from the mouth of the Winooski River along the lake shore, and rises from the water's edge to a height of 300 ft.

A large ravine in what is now downtown was filled in with refuse and raw sewage in the 19th century to make way for further development.

Neighborhoods
Burlington's neighborhoods are generally recognized by residents but have no legal or political authority.
 * Downtown: The city's commercial hub is north of Maple Street, west of South Willard Street, and mostly south of Pearl Street (as it includes all property along Pearl Street that is west of South Willard Street).
 * Hill Section: Burlington's wealthiest neighborhood is east of South Union Street and Shelburne Street, and south of Main Street, but excludes UVM and University Terrace while including all of Champlain College. The Hill Section is where the Burlington Country Club is situated.
 * The Intervale: The Intervale cannot be considered a neighborhood but is a large area encompassing many locally owned organic farms and nature preserves along the Winooski River. Located to the north of the Old North End and east of the New North End, it is included on this list because its total area is larger than that of most neighborhoods in Burlington.
 * New North End: Burlington's most populous neighborhood, a northwest suburban extension of the city, includes all points north of Burlington High School, as well as Leddy Park, Ethan Allen Park, and North Beach, and is west of Vermont Route 127 (the "Burlington Beltline").
 * Old North End: Burlington's oldest and most densely populated neighborhood is north of all property along Pearl Street, west of Hyde Street and North Willard Street, and is inclusive of areas north of Downtown and west of the University District but south of the New North End and the Intervale. It is here that Burlington's largely Jewish neighborhood known as Little Jerusalem flourished from the 1880s to the 1930s.
 * South End: A once mostly industrial and now mostly artistic district south of Downtown and west of the Hill Section, it includes the waterfront Oakledge Park and is home to the headquarters of many of Burlington's nationally known companies like Burton Snowboards and Dealer.com.
 * University District: The University District is north of the Burlington Country Club, south of the Winooski River, east of Willard Street north of Main, and east of a large chunk of the Hill Section. It includes UVM and many former single-family homes converted to student and yuppie apartments (although these are everywhere throughout the city limits and metropolitan area).

Climate
Burlington has a hot-summer humid continental climate (Köppen Dfa), with cold winters and warm, humid summers. The monthly daily average temperatures range from 29 °F in January to 76 °F in July. The annual precipitation of 43 in is well-distributed throughout the year, but the summer months are the wettest. The city's location east of Lake Champlain sometimes accounts for localized snow squalls, producing up to 13 in in 12 hours on rare occasions. Annual snowfall averages 86 in, but this figure can fluctuate greatly from one year to another. Extremes have ranged from −22.4 F on January 15, 1957, and February 12, 1979, to 104.8 F on August 11, 1944. The most recorded snowfall from a single storm is 33.1 in, which fell January 2–3, 2010.

For the Northeast United States, a heat wave is defined as having three consecutive days of 90 °F or more. There were six such heat waves from 2000–2009.

Cape May, New Jersey Geography in an ice-sheet-free world (WIP)
Based on: Cape May, New Jersey, modified by "Departures from Standard" in a Clima-Sim scenario where all Permanent Ice is replaced by Water/Pack Ice. Using standard record technique (with possible order retention) and vapor-pressure-based precipitation method.

According to the United States Census Bureau, the city had a total area of 2.90 square miles (7.50 km2), including 2.47 square miles (6.41 km2) of land and 0.42 square miles (1.10 km2) of water (14.59%). Cape May is generally low-lying; its highest point, at the intersection of Washington and Jackson Streets, is 14 ft above sea level.

Unincorporated communities, localities and place names located partially or completely within the city include Poverty Beach.

Cape May borders the Cape May County municipalities of Lower Township and West Cape May Borough, as well as the Atlantic Ocean and Delaware Bay. The Cape May–Lewes Ferry provides transportation across the Delaware Bay between North Cape May, New Jersey and Lewes, Delaware.

Cape May Harbor, which borders Lower Township and nearby Wildwood Crest allows fishing vessels to enter from the Atlantic Ocean, was created as of 1911, after years of dredging completed the harbor which covers 500 acres. Cape May Harbor Fest celebrates life in and around the harbor, with the 2011 event commemorating the 100th anniversary of the harbor's creation.

Cape May is the southernmost point in New Jersey. It is at approximately the same latitude as Washington, D.C. and Arlington, Virginia, and equidistant to Manhattan and Virginia Beach.

Climate
According to the Köppen climate classification system, Cape May, New Jersey has a humid subtropical climate (Cfa) with hot, humid summers, mild winters and year-round precipitation. Its climate resembles that of its neighbor, the Delmarva Peninsula. During the summer months in Cape May, a cooling afternoon sea breeze is present on most days, but episodes of extreme heat and humidity can occur with heat index values ≥ 100 F. During the winter months, episodes of extreme cold and wind can occur with wind chill values < 10 F. The hardiness zone of Cape May is 8b with an average annual extreme minimum air temperature of 17.0 F. The average seasonal snowfall total is around 15 in, and the average snowiest month is February which corresponds with the annual peak in nor'easter activity.

Ecology
According to the A. W. Kuchler U.S. potential natural vegetation types, Cape May, New Jersey would have a dominant vegetation type of Northern Cordgrass (73) with a dominant vegetation form of Coastal Prairie (20).

Cooler Bakersfield Climate section and weatherbox (WIP)


Bakersfield has a hot desert-type climate (Köppen BWh), with very hot, dry summers, and winters that consist of mild days with chilly/cold nights. Rainfall is low in the city, averaging only 6.5 in annually, with most of it falling in the winter. Bakersfield averages about 191 clear days a year. Bakersfield's climate makes the region suitable for growing crops ranging from carrots to citrus and almonds.

Bakersfield summers are very hot with extended stretches of hot weather and 108 days per year above 90 °F (on average between April 19 and October 12); in addition, 33 days are above 100 °F from May to September, and several days each summer can be expected to top 110 °F. Winters feature mild daytime temperatures and chilly/cold nights. Frost and/or dense fog usually occurs in winter with accompanying low visibility, causing many schools to have fog delays. Winters will usually produce a very dense layer of fog from time to time. The official time frame for tule fog to form is about 5 months long - various days from November 1 to March 31. On average, 12 mornings have freezing lows (on average between December 13 and January 26) annually, and the coldest night of the year typically bottoms out below 30 °F.

Snow is rare on the valley floor although frost may occur. The last snow fell on January 25, 1999, when the city received 6 in. The record maximum temperature was 118 °F on July 28, 1908, and the record minimum temperature was 11 °F on January 3, 1908. The most rainfall in one month was 5.82 in in December 2010, and the maximum 24-hour rainfall was 2.29 in on February 9, 1978. The wettest “rain year” has been from July 1997 to June 1998 with 14.73 in and the driest from July 1933 to June 1934 with 2.26 in.

Baghdad cooler, wetter Climate section and weatherbox (WIP)
Based on: Baghdad, curve-fit diurnal temperature variation with precipitation and fixed average lows.

Baghdad has a subtropical semi-arid climate (Köppen BSh), featuring very hot, prolonged summers and mild to cool, short winters. In the summer, from June through August, the average maximum temperature is around 37 °C, with occasional interludes around 44 °C near the ends of dry, sunny intervals in summer. Even at night, temperatures in summer are seldom below 24 °C. Baghdad's record highest temperature of 50.1 °C was reached on 28 July 2020.

Winter temperatures are typical of subtropical climates at the same latitude. From December through February, Baghdad has maximum temperatures averaging 15 to 18 C, though highs above 21 C are not unheard of. Lows below freezing occur a couple of times per year on average.

Annual rainfall, relatively evenly distributed throughout the year (of mid-latitude baroclinic origin in the winter and monsoonal origin in the summer) though with a vague summer maximum, averages 338 mm, but has been as high as 526 mm and as low as 219 mm. On 11 January 2008, light snow fell across Baghdad for the first time in 100 years. Snowfall was again reported on 11 February 2020, with accumulations across the city.

Mosul cooler, wetter Climate section and weatherbox (WIP)
Based on: Mosul, curve-fit diurnal temperature variation with precipitation and fixed average lows.

Mosul has a humid subtropical climate (Köppen Cfa), with hot, long, muggy summers, extended springs and briefer autumns with mild temperatures, and relatively cool winters. Precipitation is moderate throughout the year, with a slight summer maximum.

Comodoro Rivadavia Climate to be edited
Comodoro Rivadavia features a cold semi-arid climate (Köppen BSk). While the city receives less than 250 mm of rain annually, its relatively low evapotranspiration rate causes it to fall under this climate category. Summer is relatively hot and dry with an average temperature of 19.9 °C in January. Winter is mild with an average temperature of 6.8 °C in July. Precipitation is low, though the winter months receive more precipitation than in summer.


 * Average temperatures: Annual 12.8 °C
 * Maximum Average: January 25.6 °C
 * Minimum Average: July 2.8 °C
 * Predominant winds: W, SW
 * Precipitations: Average annual 238.7 mm
 * Month of Maximum Precipitations: May
 * Fog: 4 days/year

San Luis Río Colorado up to 0 °C July record low Climate
San-Luis-Sobre-El-Colorado has a continental desert climate (Köppen climate classification BWk) bordering closely with a continental semi-arid climate (Köppen BSk), with warm summers and cold winters; it is the coldest city in Mexico counting average annual and winter temperatures, being the only one with a daily mean in any month below freezing. The record high temperature is 38.0 °C, recorded on 25 June 1951. The record low temperature is −20.5 °C, recorded on 2 January 1950.

3.6° further south South Haven climate (WIP)
Based on: South Haven, Michigan; Escanaba, Michigan

South Haven has a humid subtropical climate (Köppen climate classification Cfa). It is generally considered to be one of the warmest areas on the coast of the Great Lakes, being on the windward side of Lake Michigan–Huron, which heavily moderates its climate. Seasonal lag is relatively pronounced, especially in autumn, with the warmest weather in late July or early August and the coolest in late January or early February. Late winter and early spring is the driest part of the year (though a secondary nadir exists in mid-summer), with supercell thunderstorms in late spring and early summer, rare subtropical storms in late summer and early autumn, and lake effect rainfall (and occasional snowfall) in late autumn and early winter.

10° further south Yongala climate
Based on: Yongala; Boulia, Queensland

Yongala has a warm-summer humid continental climate (Köppen Dfb), or a temperate highland climate (Köppen Cfb) using the -3 C coldest-month isotherm. It is situated on a high plateau and winter snow accumulation is common. The town holds several records for the lowest minimum temperature in South Australia, including a near-record low of -17.4 C on 20 July 1976 , in addition to the record low temperatures in South Australia for the months of May, June, August and September. The record warm daily minimum was 23.8 C on 24 January 1982, while the record cold daily maximum was -5 C on 15 July 1984. On average, there are 7 days per year where the maximum fails to top freezing, and the growing season lasts 75 days from mid-December to early March, prohibiting most agriculture. Frost has been recorded in every month, though it is extremely rare in January and early February and has not been recorded in all days of December, January, and February. During cold winters, the local Lake Terowie freezes over, sometimes for as long as 3 months, allowing skating and ice fishing opportunities rare in South Australia. It is also a popular area for cross-country skiing among South Australians.

10° further south Adelaide Climate section and weatherbox (WIP)
Based on: Template:Adelaide weatherbox; Birdsville

Carnarvon, Western Australia on a temperate Australia Climate
Based on: Carnarvon, Western Australia, 4.389889° further south so the Lambert Gravitational Centre is at 30 °S. Using standard solar energy temperature technique and vapor-pressure-based precipitation method.

Carnarvon has a warm semi-arid climate (BSh). Average yearly rainfall is 226 mm with the rainiest months (and the most reliable rainfall) being between May and July as the northern edges of winter cold fronts brush the region. Occasional tropical cyclones affect Carnarvon during the summer months bringing heavy rain and strong winds. Apart from this erratic source of rainfall summers are normally dry. Temperatures range from an average maximum of 33 °C in February to 22 °C in July. Average minimums are 23 °C and 11 °C respectively. The town is extremely sunny, having 211.0 clear days annually.

Bluff Knoll on a temperate Australia Climate (WIP)
Based on: Bluff Knoll, 4.389889° further south so the Lambert Gravitational Centre is at 30 °S. Using standard solar energy temperature technique and vapor-pressure-based precipitation method.

While there are no weather stations on Bluff Knoll, the Australian Bureau of Meteorology's gridded climate dataset extrapolates the highest average elevation, coldest 0.025° × 0.025° area of the Stirling Ranges (the 6.5 km2 from 34.35° to 34.375° S and 118.25° to 118.275° E; just excluding the summit but at a higher average elevation than its pixel) as having, averaged over its extent, a temperate or warm-summer mediterranean climate (Csb) according to the Köppen and Bureau of Meteorology classification systems. Alternatively, according to the Trewartha climate classification, it has a temperate oceanic climate (Do) due to insufficiently seasonal precipitation, bordering on Trewartha's humid subtropical climate (Cf) due to its eighth-warmest month (May) being only 0.5 C-change cooler than 10 C on average. Due to global warming since the 1961–1990 normals used in the temperature extrapolation, the area may now fall within that zone, but unlikely the summit itself.

Bluff Knoll is the coldest place in Western Australia. Summers are mild while winters are cold by Australian standards; area-wide winter means are comparable to those of Canberra, and average August lows at the summit likely brush freezing, with maxima frequently beating the 5.6 C state record low figure set on 16 July 1946 at Salmon Gums and 5 August 1951 at Mount Barker. Diurnal temperature variation is significantly greater in summer than in winter, averaging 12.1 C-change in January yet only 5.3 C-change in July. Like most areas of southwestern Australia, more precipitation is recorded in winter, though precipitation events tend to be heavier in summer.

Bluff Knoll is one of only a few places to experience regular snowfalls in Western Australia, with some snow reported in most years. Snow on 20 April 1970 was recorded in Bureau of Meteorology (BOM) records. A heavy snowfall was recorded on 6 October 1992 when 20 centimetres of snow fell and light snow was seen at the base, at 450 m. Snow fell on three occasions in 2016 after only falling once in 2015. A flurry was recorded on the peak after 2:00 pm on 19 April 2019—it was the earliest recorded snow event in a calendar year in the history of Western Australia.

Clockwise Yakutsk climate
Note: Using standard record technique, 13 C-change offset, and vapor-pressure-based precipitation method.

With a very continental subarctic climate (Köppen climate classification Dsc) bordering closely on a warm-summer humid continental climate (Köppen Dsb), Yakutsk experiences some of the coldest winter temperatures for any major city on Earth. The lowest temperatures ever recorded in Asia occurred in the basin of the Yana River to the northeast of Yakutsk, making it one of the coldest major cities in the world. Yakutsk is built on discontinuous permafrost, and some houses there are built on concrete piles. Yakutsk has a distinct inland location almost 1000 km from the Pacific Ocean, which coupled with the high latitude means a lack of temperature moderation, so although winters are extremely cold and long—some days in December, January, and February have never recorded above-freezing temperatures—summers are warm (though rather short), with daily maximum temperatures occasionally exceeding +30 C, making the seasonal temperature differences for the region some of the greatest in the world at 91 C-change. July temperatures soar to an above-normal average for this parallel, hotter than such southerly Far East cities as Vladivostok or Yuzhno-Sakhalinsk. The July daytime temperatures are even hotter than some marine subtropical areas. The warm summers ensure that Yakutsk is covered with a rich taiga forest with many hemiboreal species of deciduous trees.

Average monthly temperatures in Yakutsk range from +19.5 C in July to -25.6 C in January. The lowest temperature recorded in Yakutsk was -52.2 C on 5 February 1891 and the highest temperatures +38.8 C on 17 July 2011 and +38.7 C on 15 July 1942. The hottest month in records going back to 1834 has been July 1894, with a mean of +23.2 C, and the coldest, January 1900, which averaged &minus;38.4 C.

The climate is rather dry, with precipitation being relatively even throughout the year, driven by local lows and the extreme northward arm of the East Asian Monsoon in summer and extratropical cyclones sustained by the large temperature difference between the continental air and the Pacific Ocean in the winter, interspersed with generally clear periods dominated by a sporadic Siberian High. As the temperature difference and thus cyclonic activity declines in spring, generally dry conditions balanced by snowmelt result. As this occurs in the warmer "high-sun" months of the year, the climate is classified as dry-summer or even "Mediterranean" by some climate schemes (e.g. some Köppen variants), though summer proper is typically about as wet as early winter, the wettest part of the year. Still, drought conditions can occasionally persist into summer and give a Mediterranean feel, and precipitation is not very heavy in any season since the moist southeasterly winds from the Pacific Ocean lose their moisture over the coastal mountains well before reaching the Lena valley.

Typically, the first frost occurs around the September equinox, with the first accumulating snowfall and the last above freezing minima in mid-October. By early November, temperatures are consistently below freezing, which remains the case until early March. Snow depth reaches its peak near the end of March, before steeply declining and melting away almost completely by early May. The first minima above freezing occur in mid-April, and frost ends in early or mid-May. By early June, most deciduous vegetation has leafed out, and a green color is maintained until autumn begins in early-to-mid September.

With the Lena River navigable in the summer, there are various boat cruises offered, including upriver to the Lena Pillars, and downriver tours which visit spectacular scenery in the lower reaches and the Lena delta.

Clockwise Ulaangom climate
Note: Based on Ulaangom. Using standard record technique and vapor-pressure-based precipitation method.

Ulaangom has a continental semi-arid climate (Köppen BSk) relatively close to both a warm-summer humid continental climate (Köppen Dfb) and a continental desert climate (Köppen BWk), the latter of which it would be if its precipitation pattern was slightly more summer-dominant. It experiences long, very cold winters and somewhat short, warm summers. Precipitation is low, with an annual average of 167 mm. Owing to its location in a deep valley, Ulaangom is subject to temperature inversions reaching up to 13.0 C-change colder than middle and upper mountain slopes. It is thus one of the coldest places in Mongolia in the wintertime despite lying at a lower altitude than most of the country. Temperatures can reach −32 °C or lower in the winter and 35 °C or more in the summer.

Clockwise Siping Geography and climate
Note: Based on Siping, Jilin. Using 10 C-change offset and vapor-pressure-based precipitation method.

Siping is located in the transition between plains and hilly terrain, with hills to the southeast and the Songliao Plain to the northwest. The city has a four-season, monsoon-influenced, humid continental climate (Köppen Dwa), at the northern periphery of the transition zone with a humid subtropical climate (Köppen Cwa). Winters are brief (lasting from December to early March), crisp, and windy, but relatively dry, due to northerly winds with low absolute humidity, mountains from the east blocking out the influence of systems from the Sea of Japan, and intermittent Siberian Highs; the January mean temperature is -2.9 °C. Spring and fall are somewhat short, windy transitional periods, with more precipitation. Summers are hot and humid, with a prevailing southeasterly wind due to the East Asian monsoon; July averages 23.9 °C. Snow is usually light during the winter, and annual rainfall is heavily concentrated from June to August. The annual mean temperature is 11.6 °C. With monthly percent possible sunshine ranging from 46% in July to 71% in January and February, there are 2,684 hours of bright sunshine annually, with autumn and winter being especially sunny.

Clockwise Langfang Geography section (WIP)
Note: Based on Langfang. Using 10 C-change offset and vapor-pressure-based precipitation method.

Considering Langfang's position between these two prominent cities, it is a relatively green city. Every 300 to 500 m along the city's major streets are parks where local people stroll and take exercise. Langfang's five-kilometer long pedestrian street is now the longest in China. On the other hand, air pollution is a severe problem and in 2013 it was ranked among the 10 worst cities in China for air pollution, along with 6 other cities in Hebei including Xingtai, Shijiazhuang, Baoding, Handan, Hengshui and Tangshan, are among China's 10 most polluted cities.

The "Northern Three Counties" Exclave
The "Northern Three Counties of Langfang" exclave, separated from the rest of the province, is a part of Langfang City. The exclave comprises Sanhe City, Xianghe County, and Dachang Hui Autonomous County and is located between the municipalities of Beijing and Tianjin.

Climate
Langfang has a mild semi-arid climate (Köppen BSk), closely bordering a dry-winter humid subtropical climate (Köppen Cwa) and a subtropical semi-arid climate (Köppen BSh). July and August alone receive as much precipitation as all other months combined, and July receives more than all months from October to April combined. Frost occurs sporadically from early December through mid-February, for an average growing season of at least 280 days.

Clockwise Tosontsengel climate (WIP)
Note: Based on Tosontsengel, Zavkhan. Using 13 C-change offset and vapor-pressure-based precipitation method.

Tosontsengel has a subarctic climate (Köppen climate classification Dwc) with mild summers and bitterly cold winters. The average minimum temperature in January is -37.0 °C, and temperatures as low as -52.9 °C have been recorded. Most precipitation falls in the summer as rain, with some snow in the adjacent months of May and September. Winters are very dry. The wind causes the snow to drift, making it difficult for the nomadic herders to keep their animals alive.

Barometric pressure record
The highest barometric pressure ever recorded on Earth was 1085.7 mb, measured in Tosontsengel on 19 December 2001.

Alternate (Blood on the Risers?) Su-5 infobox (WIP)
Based on Sukhoi Su-5, List of jet aircraft of World War II, etc.

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Source article: Template:Infobox food

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Source article: Template:Infobox former country

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Source article: Template:Infobox military conflict

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Source article: Template:Infobox pandemic

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Source article: Template:Infobox person

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Source article: Template:Infobox planet

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Source article: Template:Infobox power station

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Source article: Template:Infobox settlement

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Source article: Template:Infobox spaceflight

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Source article: Template:Infobox television

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Source article: Template:Infobox hurricane

Template:Weather box
Source article: Template:Weather box 