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The three main factors that affect precipitation are air pressure, temperature, and humidity. Changes in these factors can impact the formation and distribution of clouds and ultimately influence when and where precipitation will occur.
The four main factors that affect precipitation are air temperature, air pressure, wind patterns, and moisture content in the air. These factors determine how much water vapor can be held in the atmosphere and where and when it will be released as precipitation.
Rock type Elevation Precipitation
The five main factors that affect the amount of runoff an area gets are precipitation intensity, soil type, vegetation cover, slope of the land, and human activities such as urbanization and deforestation. These factors influence how much water is absorbed into the ground versus how much flows over the surface as runoff.
Three main factors that affect the growth of phytoplankton are nutrient availability (such as nitrogen, phosphorus, and silica), light availability for photosynthesis, and water temperature. These factors influence the rate at which phytoplankton can photosynthesize and reproduce, ultimately impacting their growth and abundance in aquatic ecosystems.
The two main factors that affect viscosity are temperature and silica content. Higher temperatures lower viscosity while higher silica content increases viscosity.
The main cause of differences in volcanic eruption characteristics is due to the viscosity of the magma. High viscosity magmas are high in sticky silica which traps gas and produces explosive eruptions. Low viscosity magmas are low in silica and produce eruptions with far less energetic characteristics.
The temperature, composition, and gas content of the magma are the main factors that determine its viscosity. Magma with higher silica content tends to be more viscous, while higher temperatures and lower gas content can decrease viscosity. Additionally, the presence of crystal structures and mineral content within the magma can also influence its viscosity.
The three elements that determine viscosity in magma are:TemperatureSilicaOxides (gases)Viscosity changes the way in which magma will flow. Magma with low viscosity will flow much more easily than high viscosity magma.
The four main factors that affect aquatic ecosystems are waters depth, temperature, flow, and amount of dissolved nutrients.
There are several factors that affect salinity. Some of the main factors include evaporation and precipitation which will affect the salinity of oceans and seas.
poverty is the main factor that affect literacy rates
The three main factors that affect precipitation are air pressure, temperature, and humidity. Changes in these factors can impact the formation and distribution of clouds and ultimately influence when and where precipitation will occur.
There are at least 2 main factors that may affect osmosis. These 2 factors are amount of water and membrane permeability.
There are two main factors factors: gas content and magma viscosity. All magma has some amount of gas dissolved in it. This gas is released when the magma is exposed to lower pressure near the surface. In magma with a high gas content the gas bubbles out of solution and expands explosively in the presence of low pressure. If the gas content is low it may only result in a bit of bubbling. Viscosity is the tendency of a liquid to resist flowing. For example, maple syrup is more viscous than water. Magma varies in viscosity depnding on its temperature and composition. Lower temperatures and higher silica content make a more viscous magma. More viscous magmas usually have a higher gas concentration. Additionally, in viscous magmas, the gas is less likely to escape ahead of the magma in the prelude to an eruption.
The main abiotic factors that affect yellow stone national park would be hot springs, water, soil, climate and rock. These all interact with biotic factors.
The four main factors that affect precipitation are air temperature, air pressure, wind patterns, and moisture content in the air. These factors determine how much water vapor can be held in the atmosphere and where and when it will be released as precipitation.