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Hydrologic simulation is a reasonable option to assess the LID performance with respect to the water balance and is applicable to planning purposes.

The leaf anatomy of the studied taxa reflects their adaptation to conditions with an unfavorable water regime (ensures the maintenance of a normal water balance) and excessive lighting.

In general, soil water balance simulated from the model showed 50% lower cumulative drainage, 50% higher cumulative transpiration along with higher soil water retention, in PBB+R than CT.

From the soil water balance method, the annual groundwater recharge was 17,717,690 m3 which is 15.

Water use was calculated as a residual of the soil water balance.

ET is one of the main components of energy production on Earth, and it controls the water balance.

This contribution showcases a decision support approach using long term weathering time series and soil water balances with example data for turf soccer fields in six German regions.

Input data are of three types: 1) time-variable area altitude distribution (AAD); 2) time series of point water balance at long term sites (with secondary sites given in recent years); 3) weather data from nearby stations, either installed along the glacier margins or taken from a nearby site if continuous glacier-adjacent data is unavailable.

At T0 and T3, water balance, weight, lean mass (FFM), total body water (TBW), extracellular water (ECW), and nutritional and inflammatory biochemical parameters were evaluated.

The aim of the study was; (1) to investigate and analyse the differences in the surface temperature between four models of green roofs of the extensive type and a conventional roof (covered with bitumen) under the conditions of a continental climate; (2) to assess the influence of environmental parameters (climatic water balance, air temperature, relative humidity, moisture content in the profile) on changes in the temperature of the extensive type green roof profile (substrate and vegetation mat).