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Ingrid Vasilica Istrate, Sabina Macovei and Monica Bucur

Abstract

Sport represents the joy of living, to succeed, to self-exceed! Whereas the Romanian sport is at a crossroads, regarding the fewer and fewer number of children who want to practice a sport, as well as the economic situation in which it is situated, the goal of reviving the entire sports activity and to bring it to the top where Romania stayed many years in the past becomes a must. In this sense, there must be found solutions and proper strategies that lead to its revival. This issue requires a systemic approach capable to reestablish “the pyramid of sport performance” on functional principles. The present thesis is a way of organizing sports activities at club’s level, wards, groups, based on the performance pyramid, in order to achieve a high performance management, which is part of the sports reform, ranging from all of its forms, such as: human resources, financial, material, taking into account modern mechanisms (for attraction and use of resources considering the means which are available and necessary).

Open access

Pavel Ichim, Liviu Apostol, Lucian Sfîcă, Adriana-Lucia Kadhim-Abid and Vasilică Istrate

Abstract

Temperature inversions represent complex phenomena, specific for depression forms of relief which introduce changes in vertical zoning (Apăvăloae, Apostle, Pîrvulescu, 1986 by stable air stratification (Erhan, 1981), because of their morphological features, this is due to the interdependence of general movement and characteristics of the active surface, being the cause of their production (Apăvăloae, et. al., 1984, 1986, 1987). The generation of thermal inversions, their intensity and frequency is a consequence of altitude topography, morphology, fragmentation, orientation and degree of closure to external drives. (Apăvăloae, Apostle, Pîrvulescu, 1988). Thermal inversions represent complex phenomena, specific to depression landforms that introduce changes within the vertical zoning (Apăvăloae, Apostol, Pîrvulescu, 1986) by stable air stratification (Matveev, 1958, Erhan, 1981, Yinghui Liu, 2002) where vertical thermal gradient is negative (Matveev, 1958), due to their morphological features, also as a consequence of the interdependance of general circulation and characteristics of the active surface, the cause of their generation (Apăvăloae, et. al., 1984, 1986, 1987).