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Climate change in Kansas encompasses the effects of climate change, attributed to man-made increases in atmospheric carbon dioxide, in the U.S. state of Kansas. In May 2019, The Kansas City Star noted recent findings suggesting that "climate change in Kansas, Missouri and elsewhere could eventually lead to thunderstorms that are wetter and ...
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 ...
Wilson Lake is located at 38°56′25″N 98°33′24″W (38.9401464, -98.5567638) at an elevation of 1,516 feet (462 m). [4] It lies in north-central Kansas in the Smoky Hills region of the Great Plains. [5] Most of Wilson Lake lies in Russell County with a small portion of its southeastern arm extending into Lincoln County.
The soil suborders within an order are differentiated on the basis of soil properties and horizons which depend on soil moisture and temperature. Forty-seven suborders are recognized in the United States. [6] The soil great group category is a subdivision of a suborder in which the kind and sequence of soil horizons distinguish one soil from ...
Mollisol is a soil type which has deep, high organic matter, nutrient-enriched surface soil ( A horizon ), typically between 60 and 80 cm in depth. This fertile surface horizon, called a mollic epipedon, is the defining diagnostic feature of Mollisols. Mollic epipedons are created by long-term addition of organic materials derived from plant ...
Hardiness zone. A hardiness zone is a geographic area defined as having a certain average annual minimum temperature, a factor relevant to the survival of many plants. In some systems other statistics are included in the calculations. The original and most widely used system, developed by the United States Department of Agriculture (USDA) as a ...
One possible way of assessing soil thermal properties is the analysis of soil temperature variations versus depth Fourier's law, Q = − λ d T / d z {\displaystyle Q=-\lambda dT/dz\,} where Q is heat flux or rate of heat transfer per unit area J·m −2 ∙s −1 or W·m −2 , λ is thermal conductivity W·m −1 ∙K −1 ; dT / dz is the ...
AccuWeather's Wind Flow map shows a high-pressure system and Dora creating a pressure gradient, driving higher winds in Hawaii on Wednesday, Aug. 9, 2023. ... Current soil conditions vary ...