The amount and variety of changes in the water cycle triggered by anthropogenic elements relies on the amount of human impact, physiography, and the vicinity of the territory where the change happens. The changes can affect small to very large areas depending on the intensity of the factors above.
Urbanization, forestry, and plowing of small lands can largely change runoff and evaporation. Changes like this may take a long time to develop, depending on the man´s impact, and the physio-graphic features. The above listed factors are not able to have any important effects on the global eutrophication cycle.
Looking at the possible human impacts on the eurtophication cycle, the most important issues are linked with estimated anthropogenic changes in the globe's climate because of larger amounts of CO2 and more greenhouse gasses in the atmosphere. An increase to global air temperature by a few degrees could insight changes in all of the aspects of the eutrophication cycle in many different parts of the world. This could also have large impacts on the environment and socio-economic development.
Urbanization, forestry, and plowing of small lands can largely change runoff and evaporation. Changes like this may take a long time to develop, depending on the man´s impact, and the physio-graphic features. The above listed factors are not able to have any important effects on the global eutrophication cycle.
Looking at the possible human impacts on the eurtophication cycle, the most important issues are linked with estimated anthropogenic changes in the globe's climate because of larger amounts of CO2 and more greenhouse gasses in the atmosphere. An increase to global air temperature by a few degrees could insight changes in all of the aspects of the eutrophication cycle in many different parts of the world. This could also have large impacts on the environment and socio-economic development.