evapotranspiration

Examples

• All

• Lower temperatures in the other months cause less evapotranspiration, which leads to less extreme soil drying.

  Academic text (1998)

• All studies agree that South America and Africa have more evapotranspiration per unit of land area than the other continents.

  Academic text (1992)

• Average annual evapotranspiration for all land areas is nearly half that from South America.

  Academic text (1992)

• For other land areas, however, no general agreement on evapotranspiration exists.

  Academic text (1992)

• Asia has the lowest evapotranspiration rate according to two studies, Europe according to three, and Australia in two.

  Academic text (1992)

• During those months, rainfall is insufficient to offset water losses to evapotranspiration.

  Academic text (1998)

• In these low-elevation areas, forest loss will reduce evapotranspiration rates, potentially rendering these areas too wet to support trees.

  Academic text (2016)

• In North Africa, for instance, evapotranspiration would increase by 10% for each temperature increase of 1.5°C.

  Academic text (1993)

• On more local scales, urban expansion generates heat islands from concrete surfaces and reduces evapotranspiration.

  Academic text (2006)

• Terrestrial vegetation plays a crucial role in the water cycle. It modulates and sustains evapotranspiration and precipitation.

  Academic text (2010)

Surface Forms

Morphology

Etymology