run off
The condition most likely to exist in this scenario is that the soil is saturated or at field capacity. This means that the soil is holding as much water as it can and any additional precipitation will result in runoff.
The yearly total precipitation over the oceans is greater than over continents because oceans cover more of the Earth's surface and therefore have a larger area from which to receive precipitation. Additionally, the oceans are able to retain heat better than land, leading to more evaporation and subsequent precipitation. Ocean currents also play a role in transporting moisture to different regions, contributing to higher precipitation levels over oceans.
The intensity of precipitation is greater but the duration is shorter along a cold front. As a cold front moves through an area, it pushes warm air upward, leading to strong vertical uplift and intense precipitation. However, the cold front typically moves quickly, causing the precipitation to be relatively brief compared to other types of fronts.
Precip chance, short for precipitation chance, measures the likelihood of measurable precipitation occurring at a specific location within a given time frame. It is typically expressed as a percentage, where a higher percentage indicates a greater likelihood of precipitation.
An increase in temperature and precipitation would likely cause the greatest increase in chemical weathering of local bedrock. Higher temperatures speed up chemical reactions, while increased precipitation provides more water to facilitate weathering processes.
Climate ratio is used to describe the moisture side of climate. It compares the precipitation (P) with the potential evapotranspiration (Ep) for a region. One way to do this is to express the relationship between them as a ratio using the formula: Climate ratio = P / Ep When the potential evaporation is greater than yearly precipitation, this ratio is less than 1. When precipitation is greater than evapotranspiration, the ratio is greater than 1. P: precipitation (in mm) or the amount of moisture available for evapotranspiration, evapotranspiration is the combined process of evaporation and plant respiration. Ep: potential evapotranspiration (in mm) or the amount of moisture needed for evapotranspiration. This value increases as temperature and plant life increase. The climate ratios are used to determine climate type: P/Ep: Less than 0.4: arid climate 0.4 - 0.8: semiarid climate 0.8 - 1.2: subhumid climate Greater than 1.2: humid climate Source: NOAA
The condition most likely to exist in this scenario is that the soil is saturated or at field capacity. This means that the soil is holding as much water as it can and any additional precipitation will result in runoff.
soil mositure maybe recharged
The rain forest precipitation is greater that 150 cm. Rain forest precipitation is basically how much rain falls and collects on earth.
Directly. The greater the potential fall, the greater the potential energy.
True. Gravitational potential energy is directly proportional to an object's height above a reference point. This means that the greater the height of an object, the greater its gravitational potential energy.
Houston, TX
Potential energy is determined by the mass of an object and its distance from the ground. Therefore, the skydiver with greater mass will have greater potential energy when they are the same distance from the ground.
An object would have greater potential energy when positioned higher above the ground due to its increased gravitational potential energy.
in orbit.
potential
An arid or semiarid climate occurs in regions with low precipitation levels, typically less than 10-20 inches (250-500 mm) per year. These regions often experience high temperatures and have limited vegetation due to the lack of moisture.