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Ohio is expected to experience greater amounts of precipitation, but less snowfall in the winter due to the higher temperatures. [1] Accordingly, the risk of flooding in Ohio is due to increase. [2] Greater heavy rainfall in the Midwest are leading to soil erosion and nutrient loss. [4]
Photograph taken 21 March 2010 in Norwich, Vermont. Frost heaving (or a frost heave) is an upwards swelling of soil during freezing conditions caused by an increasing presence of ice as it grows towards the surface, upwards from the depth in the soil where freezing temperatures have penetrated into the soil (the freezing front or freezing boundary).
The warmer weather in Ohio might have you itching to start some yardwork. But is it the best time of year to spread grass seed or fertilize the lawn?
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.
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Very intense chemical weathering, leaching, and erosion in warm and humid regions where soil does not freeze; Climate directly affects the rate of weathering and leaching. Wind moves sand and smaller particles (dust), especially in arid regions where there is little plant cover, depositing it close to [55] or far from the entrainment source. [56]
There have been 12 past moderate to strong El Niño events between 1950 and 2022.