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The phrase "mesonet" is a portmanteau of the words mesoscale and network. The network consists of 120 automated stations covering Oklahoma and each of Oklahoma's counties has at least one station. At each site, the environment is measured by a set of instruments located on or near a 10-meter (33 ft)-tall tower.
In meteorology and climatology, a mesonet, portmanteau of mesoscale network, is a network of automated weather and, often also including environmental monitoring stations, designed to observe mesoscale meteorological phenomena and/or microclimates. [ 3][ 4] Dry lines, squall lines, and sea breezes are examples of phenomena observed by mesonets.
The following is a list of stations owned or operated by Sinclair Broadcast Group. Sinclair owns or operates 294 television stations across the United States in 89 markets ranging in size from as large as Washington, D.C. to as small as Ottumwa, Iowa / Kirksville, Missouri. [ 1] Several of these stations are owned by affiliate companies with ...
A taxonomy is an arrangement in a systematic manner; the USDA soil taxonomy has six levels of classification. They are, from most general to specific: order, suborder, great group, subgroup, family and series. Soil properties that can be measured quantitatively are used in this classification system – they include: depth, moisture ...
The physical properties of soil, in order of decreasing importance for ecosystem services such as crop production, are texture, structure, bulk density, porosity, consistency, temperature, colour and resistivity. [ 1] Soil texture is determined by the relative proportion of the three kinds of soil mineral particles, called soil separates: sand ...
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The thermal properties of soil are a component of soil physics that has found important uses in engineering, climatology and agriculture. These properties influence how energy is partitioned in the soil profile. While related to soil temperature, it is more accurately associated with the transfer of energy (mostly in the form of heat ...
The frost line —also known as frost depth or freezing depth —is most commonly the depth to which the groundwater in soil is expected to freeze. The frost depth depends on the climatic conditions of an area, the heat transfer properties of the soil and adjacent materials, and on nearby heat sources. For example, snow cover and asphalt ...