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Abstract

In the summer of 1983 and 1984 some atmospheric diffusion experiments were carried out at the Montalto di Castro site, in the presence of a sea breeze, using a chemical tracer (SF-6). The results showed the effect of the strong directionality of breeze circulation during the warmest period of the day: the limitation in vertical diffusion, caused by the development of the Internal Boundary Layer (I.B.L.), was perfectly shown by the vertical thermal soundings which were performed at the same time as the SF-6 emission.

Additional information

Authors: BASSETTI D, JRC ISPRA ESTAB. (ITALY);ENEA, CRE-CASACCIA (ITALY);CAGLIONE P, JRC ISPRA ESTAB. (ITALY);ENEA, CRE-CASACCIA (ITALY);CAGNETTI P, JRC ISPRA ESTAB. (ITALY);ENEA, CRE-CASACCIA (ITALY);PELLEGRINI A JRC ISPRA ESTAB. (ITALY), JRC ISPRA ESTAB. (ITALY);ENEA, CRE-CASACCIA (ITALY);ENEA, CRE-CASACCIA (ITALY), JRC ISPRA ESTAB. (ITALY);ENEA, CRE-CASACCIA (ITALY)
Bibliographic Reference: EUR 10630 EN (1986) MF, 133 P., BFR 300, BLOW-UP COPY BFR 675, EUROFFICE, LUXEMBOURG, POB 1003
Availability: Can be ordered online
Record Number: 1989125004500 / Last updated on: 1987-01-01
Category: PUBLICATION
Available languages: en