Examines airflow in the Glowworm cave of New Zealand using conventional methods together with experimental procedures using SF6 and CCL2F2 tracer gases. Results show that the rate and direction of airflow are a direct response to a thermally
Cave climate: assesment of airflow and ventilation.
Year:
1982
Bibliographic info:
Journal of Climatology vol 2. 1982 p.383-397 13 figs. 1 tab. 8 refs. #DATE 01:01:1982 in English