The back-and-forth movement of living and non-living matter used in the production of living matter

The back-and-forth movement of living and non-living matter used in the production of living matter is the biogeochemical cycle. It is a pathway by which a chemical substance moves through both biotic (biosphere) and abiotic (lithosphere, atmosphere, and hydrosphere) components of Earth.

Explanation:

A biogeochemical cycle or material turnover or cycling of substances is a pathway by which a synthetic substance moves within biotic (biosphere) and abiotic (lithosphere, atmosphere, and hydrosphere) sections of Earth.The most significant biogeochemical cycles are the carbon cycle, nitrogen cycle, oxygen cycle, phosphorus cycle, and the water cycle. The biogeochemical cycles perpetually have a state of stability.

relative humidity, temperature and dew point -- are bound together in the mathematical relationship below. relative humidity changes when temperatures change. because warm air can hold more water vapor than cool air, relative humidity falls when the temperature rises if no moisture is added to the air. so i would say a