The city of Tulsa lies along the Arkansas River at an elevation of
700 feet above sea level. The surrounding terrain is gently rolling.
At latitude 36 degrees, Tulsa is far enough north to escape the long
periods of heat in summer, yet far enough south to miss the extreme cold
of winter. The influence of warm moist air from the Gulf of Mexico is
often noted, due to the high humidity, but the climate is essentially
continental characterized by rapid changes in temperature. Generally
the winter months are mild. Temperatures occasionally fall below zero
but only last a very short time. Temperatures of 100 degrees or higher
are often experienced from late July to early September, but are usually
accompanied by low relative humidity and a good southerly breeze. The
fall season is long with a great number of pleasant, sunny days and cool,
bracing nights.
Rainfall is ample for most agricultural pursuits and is distributed
favorably throughout the year. Spring is the wettest season, having an
abundance of rain in the form of showers and thunderstorms.
The steady rains of fall are a contrast to the spring and summer
showers and provide a good supply of moisture and more ideal conditions
for the growth of winter grains and pastures. The greatest amounts of
snow are received in January and early March. The snow is usually light
and only remains on the ground for brief periods.
The average date of the last 32 degree temperature occurrence is late
March and the average date of the first 32 degree occurrence is early
November. The average growing season is 216 days.
The Tulsa area is occasionally subjected to large hail and violent
windstorms which occur mostly during the spring and early summer, although
occurrences have been noted throughout the year.
Prevailing surface winds are southerly during most of the year. Heavy
fogs are infrequent. Sunshine is abundant. The prevalence of good flying
weather throughout the year has contributed to the development of Tulsa as
an aviation center.