. . . "0899-8418" . "RIV/00216224:14310/12:00057194" . . "Airflows and their impact on microclimatic parameters were studied in the two entranced C\u00EDsa\u0159sk\u00E1 Cave (Moravian Karst, Czech Republic). Basing on the airflow direction with respect to the upper entrance (UE) and lower entrance (LE), three ventilation modes were distinguished: upward airflow one (UAF mode), downward airflow one (DAF mode), and transitional mode. A switching between the UAF and DAF happens in the transitional mode, in the range of external temperatures from 9.5 to 11.1 C. Basing on the extent of cave ventilation, a period of active ventilation and period of stagnant ventilation were recognised. The cave air is intensively exchanged with external airs during the active ventilation period when the cave persists in either the DAF or UAF mode. During the stagnant ventilation period, the single airflow modes switch during diurnal cycle and only cave entering passages are vented (impacted)." . "4" . . . . "International Journal of Climatology" . . . . "Air circulation and its impact on microclimatic variables in the C\u00EDsa\u0159sk\u00E1 Cave (Moravian Karst, Czech Republic)" . . "3"^^ . "Novotn\u00FD, Roman" . "14310" . "32" . "000301494600010" . "Air circulation and its impact on microclimatic variables in the C\u00EDsa\u0159sk\u00E1 Cave (Moravian Karst, Czech Republic)"@en . "Troppov\u00E1, Dana" . "[B77DDC62D3D3]" . "Airflows and their impact on microclimatic parameters were studied in the two entranced C\u00EDsa\u0159sk\u00E1 Cave (Moravian Karst, Czech Republic). Basing on the airflow direction with respect to the upper entrance (UE) and lower entrance (LE), three ventilation modes were distinguished: upward airflow one (UAF mode), downward airflow one (DAF mode), and transitional mode. A switching between the UAF and DAF happens in the transitional mode, in the range of external temperatures from 9.5 to 11.1 C. Basing on the extent of cave ventilation, a period of active ventilation and period of stagnant ventilation were recognised. The cave air is intensively exchanged with external airs during the active ventilation period when the cave persists in either the DAF or UAF mode. During the stagnant ventilation period, the single airflow modes switch during diurnal cycle and only cave entering passages are vented (impacted)."@en . . . . "4"^^ . . . "US - Spojen\u00E9 st\u00E1ty americk\u00E9" . "Air circulation and its impact on microclimatic variables in the C\u00EDsa\u0159sk\u00E1 Cave (Moravian Karst, Czech Republic)" . . . "I, P(GA205/03/1128), Z(MSM 143100004), Z(MSM0021622412)" . . . . . "airflow; cave; CO2; humidity; oscillations; temperature; ventilation mode; ventilation period"@en . "Bald\u00EDk, V\u00EDt" . . "121377" . "25"^^ . "RIV/00216224:14310/12:00057194!RIV13-GA0-14310___" . . . . "10.1002/joc.2298" . . "Faimon, Ji\u0159\u00ED" . "Air circulation and its impact on microclimatic variables in the C\u00EDsa\u0159sk\u00E1 Cave (Moravian Karst, Czech Republic)"@en .