Continentality
Encyclopedia
Continentality is the tendency of land to experience more thermal variation than water, due to the land's lower specific heat capacity. Continental climate
also tends to be dryer than oceanic climate
as there is less moisture input to the atmosphere from evaporation. Because temperature and moisture content are key factors in influencing regional climate, continentality affects and influences both temperature
and precipitation
.
This causes localised as well as global effects on weather patterns. For instance, high pressure caused by cold, sinking air over Siberia
in winter and low pressure caused by warm, rising air over Siberia in summer help drive the monsoons of South Asia.
A characteristic of regions that lack the temperature moderating effects of the sea and that exhibit a greater range of minimum and maximum temperature, both daily and annually.
The sea itself has its own weather pattern. Winds and currents range depending on the ocean. Land near the sea share its patterns, whereas further away the land begins to develop its own weather patterns.
Continentality is the reverse of water moderation
. Mean daily range (MDR), the difference between the mean maximum and the mean minimum temperatures, estimates continentality.
Temperatures in continental sites are more variable and extreme. In summer, continental sites receive more heat to assist fruit and vine maturation, but they also have increased hazard from other related weather events characteristics of continental sites which interfere with grapevine function.
cold hardiness.
Where MDR is high, the probability of spring freeze increases. In the spring when the temperature is 50°F or more, buds begin to develop. High MDR sites experience more frequent high temperatures which promote early bud growth and more frequent low temperatures which may cause freeze injury. The primary benefit of water moderation to NY sites is reduced winter cold hazard. The water moderation provides an additional benefit of reduced low spring and fall freeze hazard. More continental sites may require freeze protection (sprinkle irrigation, wind machines or heaters) in the spring, early summer and fall to prevent freeze injury to green tissues.
Low temperature hazard is primarily related to latitude
. At northern latitudes water moderation is required for winter cold moderation. Northern European vine production benefits from the moderating influence of the Atlantic Ocean
and especially of the Gulf Stream
. (Note relatively high December, January and February expected monthly low temperatures in Bordeaux France relative to the North American sites, and that the very continental Fairmont, MN, also stands out as having more extreme temperatures. In the latter case the problem is both variable temperatures and low total heat supply.) Water moderation that reduces continentality facilitates grape production at higher latitudes.
Continental climate
Continental climate is a climate characterized by important annual variation in temperature due to the lack of significant bodies of water nearby...
also tends to be dryer than oceanic climate
Oceanic climate
An oceanic climate, also called marine west coast climate, maritime climate, Cascadian climate and British climate for Köppen climate classification Cfb and subtropical highland for Köppen Cfb or Cwb, is a type of climate typically found along the west coasts at the middle latitudes of some of the...
as there is less moisture input to the atmosphere from evaporation. Because temperature and moisture content are key factors in influencing regional climate, continentality affects and influences both temperature
Temperature
Temperature is a physical property of matter that quantitatively expresses the common notions of hot and cold. Objects of low temperature are cold, while various degrees of higher temperatures are referred to as warm or hot...
and precipitation
Precipitation (meteorology)
In meteorology, precipitation In meteorology, precipitation In meteorology, precipitation (also known as one of the classes of hydrometeors, which are atmospheric water phenomena is any product of the condensation of atmospheric water vapor that falls under gravity. The main forms of precipitation...
.
This causes localised as well as global effects on weather patterns. For instance, high pressure caused by cold, sinking air over Siberia
Siberia
Siberia is an extensive region constituting almost all of Northern Asia. Comprising the central and eastern portion of the Russian Federation, it was part of the Soviet Union from its beginning, as its predecessor states, the Tsardom of Russia and the Russian Empire, conquered it during the 16th...
in winter and low pressure caused by warm, rising air over Siberia in summer help drive the monsoons of South Asia.
A characteristic of regions that lack the temperature moderating effects of the sea and that exhibit a greater range of minimum and maximum temperature, both daily and annually.
The sea itself has its own weather pattern. Winds and currents range depending on the ocean. Land near the sea share its patterns, whereas further away the land begins to develop its own weather patterns.
Continentality is the reverse of water moderation
Oceanic climate
An oceanic climate, also called marine west coast climate, maritime climate, Cascadian climate and British climate for Köppen climate classification Cfb and subtropical highland for Köppen Cfb or Cwb, is a type of climate typically found along the west coasts at the middle latitudes of some of the...
. Mean daily range (MDR), the difference between the mean maximum and the mean minimum temperatures, estimates continentality.
Temperatures in continental sites are more variable and extreme. In summer, continental sites receive more heat to assist fruit and vine maturation, but they also have increased hazard from other related weather events characteristics of continental sites which interfere with grapevine function.
Water moderates both summer and winter temperatures
Water moderation (less continentality, lower MDR) increases the length of the growing season. In the fall, continental sites have greater temperature fluctuation meaning higher day temperatures and lower night temperatures. This aids fruit maturation, but should the temperature drop below 28°F, foliage is killed and the season is abruptly terminated. This not only interferes with fruit maturation, but it can prevent the achievement of potential grapevineGrapevine
Grapevine is the common name for plants of the genus Vitis. Other meanings include:*Grapevine , a term often used to describe a form of communication by means of gossip or rumor, as in "heard it through the grapevine"...
cold hardiness.
Where MDR is high, the probability of spring freeze increases. In the spring when the temperature is 50°F or more, buds begin to develop. High MDR sites experience more frequent high temperatures which promote early bud growth and more frequent low temperatures which may cause freeze injury. The primary benefit of water moderation to NY sites is reduced winter cold hazard. The water moderation provides an additional benefit of reduced low spring and fall freeze hazard. More continental sites may require freeze protection (sprinkle irrigation, wind machines or heaters) in the spring, early summer and fall to prevent freeze injury to green tissues.
Low temperature hazard is primarily related to latitude
Latitude
In geography, the latitude of a location on the Earth is the angular distance of that location south or north of the Equator. The latitude is an angle, and is usually measured in degrees . The equator has a latitude of 0°, the North pole has a latitude of 90° north , and the South pole has a...
. At northern latitudes water moderation is required for winter cold moderation. Northern European vine production benefits from the moderating influence of the Atlantic Ocean
Atlantic Ocean
The Atlantic Ocean is the second-largest of the world's oceanic divisions. With a total area of about , it covers approximately 20% of the Earth's surface and about 26% of its water surface area...
and especially of the Gulf Stream
Gulf Stream
The Gulf Stream, together with its northern extension towards Europe, the North Atlantic Drift, is a powerful, warm, and swift Atlantic ocean current that originates at the tip of Florida, and follows the eastern coastlines of the United States and Newfoundland before crossing the Atlantic Ocean...
. (Note relatively high December, January and February expected monthly low temperatures in Bordeaux France relative to the North American sites, and that the very continental Fairmont, MN, also stands out as having more extreme temperatures. In the latter case the problem is both variable temperatures and low total heat supply.) Water moderation that reduces continentality facilitates grape production at higher latitudes.