In this paper, the climatic aspects of the area of Langovet, a village located in the immediate vicinity of the border with Serbia, were presented in the period of 2018-2020, and the data used in this study were provided by CMR Banat Ctisana, based in Timisoara. The movement of sub-Mediterranean air masses leads to their channeling on the Danube corridor where it is also known as Coşava or locally Năidăşan. The effects of this circulation condition the sudden melting of snow during the winter, reflected by small increases in level but which occur over a short period of time. The air temperature is a basic element in characterizing the climate under the ratio of values, variables, averages and extremes. Regarding the average annual temperature of the area, we mention that it is higher. The average annual isotherm of 110 delimits the corridor of the Danube, and thanks to these evaluations we signal the presence of biocenoses specific to the area. Particularly intense air currents develop in this region, of the „bora” type, locally called „Coşava”. The „Coşava” wind has a turbulent character, and according to the wind rose, the predominant directions are east and west. The speed can reach up to 85 km/h, with gusts up to about 140 km/h and 145 km/h, with an average duration of up to one day, sometimes even two days. Approximately half of the days of the year are windy, the other days presenting an atmospheric calm, a fact that is of particular importance in the context of „green energy”, as a source of renewable energy.