When Does It Snow in Oklahoma?

When Does It Snow in Oklahoma? We all have wondered when our favorite city sees snow, but how much does it really fall each year? We’ve found the average annual snowfall for Oklahoma City and the western panhandle. Read on to learn about Oklahoma’s northeastern corner and the winter climate there. In addition, you can find out what the weather is like in each area. If you’re wondering, “When Does It Snow in Oklahoma?“, this article can help!

Average annual snowfall in Oklahoma City

Oklahoma City gets about 2.1 inches of snow on average each January. However, this month doesn’t come as often as others, and the city has a snowless period of 9.1 months from February 22 to November 25. The region around northeast Oklahoma is most likely to experience an eight-inch snowfall during the winter months. This is due to changes in elevation, which makes winters in this area more likely than those in other areas of the state.

The wettest month in Oklahoma City is May, followed by January. There are 79.1 days of rain per year, with a 29% chance of rain during Summer. The average annual snowfall in Oklahoma City is 5.8 inches. Winters are drier than summers, with only four months seeing significant amounts of snowfall. There are also two dry seasons and two rainy ones in the region. During the latter, temperatures rise during May and January are often very warm.

Although the climate is generally temperate in Oklahoma City, the weather changes quickly. Temperatures can remain in the low 90s through mid-October, but the temperatures can drop as low as -8 degrees Fahrenheit in November. On September 26, the last 90 degF (32 degrees Celsius) of the warm season is expected. In contrast, Phoenix Arizona experiences temperatures that are over 99 degrees Fahrenheit for more than 107 days a year.

While snow is rare in Oklahoma City, the city is still blessed with a climate that is favorable most of the year. This is an excellent climate for residents, and prolonged periods of rain and bad weather are almost unheard of. The average temperature in Oklahoma City is 16.7 degC/62.0 degrees F. There is approximately 860 mm of precipitation per year in Oklahoma City. The least precipitation falls in January, with just 38 mm/1.5 inches falling on the ground. Most of it falls in May.

The first measurable snowfall in Oklahoma City occurs on December 17th. Since 1990, there have been five first snowfalls in Oklahoma City. On January 1st, however, the first snowfall occurs only 23% of the time. This makes Oklahoma City’s winters much more pleasant than most parts of the U.S. When it does snow in Oklahoma City, it’s likely to be a deep powdery mess.

In addition to the average snowfall, there are other precipitation factors to consider. Oklahoma City is situated in a zone of conflict between cold dry air from Canada and warm moist air from the Gulf of Mexico. These differences cause strong to severe thunderstorms to form in central Oklahoma. During the spring season, precipitation increases, but is often accompanied by a significant amount of severe weather. Rainfall is at its highest from mid-April to early June.

Average annual snowfall in the western panhandle

The snowfall averages in the western and central panhandles of Texas vary greatly. In Amarillo, the snowiest date was September 29, 1984, but other cities in the state recorded snow in September. While it melted in the process, the snow fell in the city of Kenton on September 18, 1971, and Stratford on September 27, 1936. Average annual snowfall in the western and central panhandle of Texas is 17.9 inches, with a trace of snow as far east as Canadian.

Depending on location, the average snowfall can range from under two inches in the southern half of the state to more than 30 inches in the western panhandle. While the precipitation averages are lower in western Oklahoma than in eastern Oklahoma, the snowfall amount can vary significantly throughout the state. For instance, during the summer months, the rain is generally below normal and the rains tend to fall in July and August.

While the southern portion of the state will stay warm and dry, the western half will remain cold and wet. The first freeze of spring in Oklahoma generally falls around mid-December and can occur as late as the first week of April. However, the last freeze of spring in the western panhandle may occur as late as the last week of April. Historically, freezing temperatures have occurred as late as April 20 along the southern border, and as late as mid-April in northwest Oklahoma.

In the winter, Oklahoma City experiences between six to eight inches of snow. Those values can vary widely, but the average is about eight inches. The highest 24-hour total in Oklahoma was recorded in March. The US average snowfall in winter is 28 inches, so Oklahoma City and the western Panhandle of Oklahoma have the highest snowfall on average. But, despite the high temperatures, winter isn’t all bad for this region.

In the southeast of the state, temperatures seldom drop below 32 degrees. Throughout the panhandle, the average is about fifteen days below that mark. In the western half of the state, it is a much different story. On average, temperatures are about sixty degrees Fahrenheit (or 16 degrees Celsius). The eastern half of the state gets less than fifteen days of triple-digit temperatures. And it’s rare to see more than one hundred-degree year, which is about one in every seven years.

While temperatures are generally warm in winter in Oklahoma, the state also experiences some of the highest rainfall. Winter temperatures in Oklahoma fall below zero during October and April. Temperatures can drop below freezing during these months, and the coldest part of the state experiences more than 130 below-freezing days a year. Almost every winter, Oklahoma sees snowfall. The snowy season peaks in December and February. The first major snowfall is usually in December. Snowfall in Oklahoma typically peaks between December and February.

Average annual snowfall in the northeastern corner of the state

The average amount of snowfall in the state of Oklahoma varies by location. The eastern Panhandle averages less than six inches of snow per year, while the western Panhandle averages more than thirty inches. The average snowfall in Oklahoma is greater in the northeast and northwest corners of the state, while it is less common in central and southeastern Oklahoma. However, ice cover can make travel in all parts of Oklahoma dangerous.

Precipitation in Oklahoma varies by season and region. The eastern half of the state experiences the climatological maximum, occurring in May. In contrast, precipitation during the summertime is largely convective, produced by mesoscale systems. It is uncommon to see measurable snowfall during the summertime. Most of the snowfall occurs in the late afternoon and early evening, primarily due to severe thunderstorms.

The western half of the state, excluding the panhandle, has the highest average temperature. In the northeastern corner, it is 56 degrees. In contrast, the eastern half experiences less than 15 triple digit days, with a range of 35 degrees in the south and twenty in the northeast. In the southwestern portion, only one out of seven years has temperatures in the low to mid-twenties.

Located in the West South Central region, the northeastern corner of Oklahoma is characterized by continental climate. The Gulf of Mexico brings warm, moist air to the north. The summer is hot and humid, while winters are short. The spring season is often plagued by tornadoes. Winters are typically short and have little snowfall, although there are times when cold temperatures can become extreme.

In the northwest, the date for the first freeze is usually late March or early April. In the east, it usually takes until April 15 before the last freeze. However, this date varies considerably, with the northern area having a late freeze. However, in the western part of the state, freezing temperatures may occur as early as the first week of May. This is especially true for areas near the Missouri border.

Some regions of the state have higher than normal snowfall. In contrast, the southern portion of the state has lower average snowfall. This is probably due to a change in measurement technique. In the first half of the decade, 11 of the 40 sites saw the most snowfall, whereas only nine of the forty saw the lowest amounts. The most recent decade lasted only nine years, which may be due to a change in measurement method