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ECONOMICS VS RELIGION AMERICAN COLONIES	5 days ago · HYDROLOGIC EFFECTS OF URBAN DEVELOPMENT Streams are fed by runoff from rainfall and snowmelt moving as overland or subsurface flow. Floods occur when large volumes of runoff flow quickly into streams and rivers. The peak discharge of a flood is influenced by many factors, including the intensity and duration of storms and snowmelt, the topography and geology of stream . Irrigation is the process of applying controlled amounts of water to plants at needed intervals. Irrigation helps to grow agricultural crops, maintain landscapes, and revegetate disturbed soils in dry areas and during periods of less than average rainfall. Irrigation also has other uses in crop production, including frost protection, suppressing weed growth in grain fields and preventing soil. 6 days ago · Forecasters are predicting Iota to bring a life-threatening storm surge 15 to 20 feet above normal tide levels to the impact area, where it is also thought to incur 8 to 16 inches of rain with.

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All of this extra carbon needs to go somewhere. So far, land plants and the ocean have taken up about 55 percent of the extra carbon people have put into the atmosphere while about 45 percent has stayed in the atmosphere.

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Eventually, the land and oceans will take up most of the extra carbon dioxide, but as much as 20 percent may remain in the atmosphere for many thousands of years. The changes in the carbon cycle impact each reservoir.

Excess carbon in the atmosphere warms the planet and helps plants on land grow more. Excess carbon in the ocean makes the water more acidic, putting marine life in danger. Carbon dioxide, methane, and halocarbons are greenhouse gases that absorb a wide range of energy—including infrared energy heat emitted by the Earth—and then re-emit it. The re-emitted energy travels out in all directions, but some returns to Earth, where it heats the surface.

Without greenhouse gases, Earth would be a frozen degrees Celsius 0 degrees Fahrenheit. With too many greenhouse gases, Earth would be like Venus, where the greenhouse atmosphere keeps temperatures around degrees Celsius Fahrenheit. Rising concentrations of carbon dioxide are warming the atmosphere. The increased temperature results in Efgect evaporation rates and a wetter atmosphere, which leads to a vicious cycle of further warming. Because scientists know which wavelengths of energy each greenhouse gas absorbs, and the concentration of the gases in the atmosphere, they can calculate how much each gas contributes to warming the planet.

The rest is caused by small particles aerosols and minor greenhouse gases like methane. Warmer temperatures evaporate more water from the oceans, expand air masses, and lead to higher humidity. Cooling causes water vapor to condense and fall out as rain, sleet, or snow.

Effects of Changing the Carbon Cycle

Carbon dioxide, on the other hand, remains a gas at a wider range of atmospheric temperatures than water. Carbon dioxide molecules provide the initial greenhouse heating needed to maintain water vapor concentrations. When carbon dioxide concentrations drop, Earth cools, some water vapor falls out of the atmosphere, and the greenhouse warming caused by water vapor drops.

Likewise, when carbon dioxide concentrations rise, air temperatures go up, and more water vapor evaporates into the atmosphere—which then amplifies greenhouse heating.]