The objectives of this work are: a) to undestand how the air temperature and relative humidity in Basin B of Núcleo Cunha (IF) relate to micro and topoclimatic controls (altitude, gradient, slope orientation, vegetation, sky diagram, etc.); b) to comprehend the relative importance of each micro and topoclimatic control in the air temperature and relative humidity variation within different
... [Show full abstract] atmospheric systems.
Micro and topoclimatic controls influence temperature and relative humidity variation differently in each atmospheric system. However, the arrangement of some specific climatic controls generates environments that conserve the rhythm of temperature and relative humidity, whatever the atmospheric system. Water in the soil has an evident role in the reduction of temperature and relative humidity variation. Vegetation has a fundamental role in the maintenance of the relative humidity, being clearly more importante than gradient and slope orientation.
Climatic units of Basin B were delimited as a synsthesis of all interactions. The concept of climate units as a space where climatic attributes and controls keep a relative homogeneity, made possible the identification of four topoclimates and several microclimates units.