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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
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The product of the numerator of one ratio and the denominator of ratio?
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How can you use the calculation of the climate ratio to determine the climate type?
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What important feature of climate is not described by the climate ratio?
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Which is correctly compared to oxygen isotopes 16O and 18O?
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What is the antifreeze ratio for a 2003 gmc sierra?
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What type of ratio is 12 is?
12 is a single number. In so far as it can represent a ratio, it is a ratio of 12 to 1: a unit ratio.12 is a single number. In so far as it can represent a ratio, it is a ratio of 12 to 1: a unit ratio.12 is a single number. In so far as it can represent a ratio, it is a ratio of 12 to 1: a unit ratio.12 is a single number. In so far as it can represent a ratio, it is a ratio of 12 to 1: a unit ratio.
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What is the mass ratio of pennies to nickels?
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What layers of rock can tell us about the climate when the rocks were forming?
Different types of rock layers, such as sedimentary rocks like limestone or sandstone, can provide information about past climates based on the fossils they contain. For example, the presence of tropical plant fossils in certain layers indicates a warm climate. Additionally, the ratio of certain isotopes in rocks can also provide clues about past temperatures and climate conditions.
