"climatic balance" is a correct and usable phrase in written English.
It is most often used to refer to a state of equilibrium in the global climate system, often characterized by the absence of extreme weather conditions. For example, "Environmental scientists are striving to maintain a steady climatic balance in order to protect the planet's future."
The British government is to permit the desecration of upland and coastal Britain in the hope that this will shift the climatic balance of Planet Earth.
Moreover, because all salt lakes are dependent on a climatic balance, they are a great deal more sensitive to long-term climatic changes than are freshwater lakes.
In the majority of computer projections, continued human destruction of the forest tends to push the climatic balance in the region in a direction that makes the dieback situation more likely.
The final set of predictors represented topography (altitude standard deviation, ALT_STD), temperature (MST; mean winter temperature, MWT), seasonal and overall climatic water balance (WB_SUM; annual water balance, WBAL) and human impact (human footprint, HFOOTP; Table 1).
(°C) 22.9 22.8 24.2 24.0 Summer precipitation (mm) 210 215 180 188 Climatic water balance (mm) −90.5 −157.8−147.2 −147.2 Climatic water balance is the difference of precipitation and evapotranspiration for grass.
Crimmins, S. M., Dobrowski, S. Z., Greenberg, J. A., Abatzoglou, J. T. & Mynsberge, A. R. Changes in climatic water balance drive downhill shifts in plant species' optimum elevations.
Climatic water balance and soil moisture conditions do not favor leaching of nitrates from the small amount of fertilizer-N applied to Oxisols and Ultisols in Latin America.
For decision support on landscape renovation and land rededication by afforestation in NE Germany the seepage reduction under forest is to be taken into consideration, especially with respect to the conservation or restoration of wetlands in regions with negative climatic water balance.
Climatic water balance, furthermore, is the difference between the precipitation and the potential evapotranspiration of grass.
The climatic water balance indicates a higher aridity in the two eastern regions Fläming and Oder-Spree compared to the two western regions.
For this purpose, water available to plants (wap) is estimated as the sum of climatic water balance (cwb) in the growing season and the available soil moisture (asm).
