tea often exhibit many desirable features
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Climate with some seasonality. The seasonality of precipitation is important to influence the quality of tea, and tea leaves harvested at different times will produce a finished product with very different characteristics. The seasonality is, therefore, an asset in the production of tea, which explains why most of the well-known tea-producing regions have strongly seasonal climates. Seasonality can include a simple dry dry pattern such as Asian monsoon, or a bimodal precipitation pattern, with two different wet stations and two different dry seasons in each year, as occurs in parts of Sri Lanka and Kenya. Diagram that explains the orographic elevator
The orographic elevation explains much of the influence of elevation in precipitation.
Elevation influences the climate.
Elevation or altitude is one of the largest local or regional influencers of climate. As it rises at a higher elevation, temperatures become more variable, precipitation usually becomes higher, but moisture becomes lower. This is due to a series of processes, one of the most important of which is called orographic elevation.
Organic uprising described.
BEC The phenomenon of what happens when the air rises. At higher altitudes, air pressure is lower, so air expands, and the expansion process cools air. The air capacity to hold the water vapor depends on the temperature, and is lower at lower temperatures. Therefore, as air increases, it expands and cooled, and can not keep all its humidity, so this causes clouds, and often cause rainfall, such as rain or snow. The orographic elevation explains why the mountains side of the mountains has a rain from the mountains and the side of the other side of the other side of the wind), the side of the mountains tends to be dry, a phenomenon called rain shadow . Tea, a water loving plant, tends to be cultivated on the windward sides of the mountain ranges.
A tea garden on a hill, with dense fog and tea plantation of height trees in Ooty, India, a region that reaches more than 7000 feet in height. Photo of Vinrox, with license under CC BY-SA 3.0.
The tea plant often can only be cultured within a certain range of altitudes. Although large tea often exhibit many desirable features and sometimes get a higher price than the
R low altitude counterparts, on ascending at progressively high altitudes, there is a point beyond which conditions are cooled too much to cultivate the tea plant. The highest commercial tea operations are around 8000 feet (approximately 2400 m) in elevation. As one travels further from Ecuador, and in colder and colder climates, the highest possible elevation to which the tea plant can be grown becomes lower.
Moisture moderates the climate
Water holds heat better than any other common substance in our environment. Both bodies of water, such as the ocean or large lakes, as well as water vapor in the air, have a considerable amount of heat. A dry region can be heated and cooled quickly, while the regions that have more water tend to heat up and cool more slowly. Water moderates thus temperatures in a region. The phenomenon of the water moderation climate explains how there may be two commercial tea operations in the United States, in a region it is usually considered too cold to grow tea: both are near the water, one in coastal South Carolina, moderate by The Atlantic Ocean and the other I
