Water vapour and greenhouse effect

Title (Dublin Core)

eng Water vapour and greenhouse effect

hrv Vodena para i efekt staklenika

Description (Dublin Core)

eng Water content of the atmosphere and its role in the greenhouse effect is investigated. Values of solar constant measured by satellite Nimbus-7 channel 100 have been used for calculating effective temperature of the atmosphere by Stefan- Boltzmann's law. The greenhouse effect is defined as the difference between the surface temperature and the atmosphere effective temperature. The yearly variation of greenhouse intensity was calculated. It was found that relation between greenhouse intensity and water vapor content is logarithmic.

hrv Proučene su količina i uloga vodene pare u atmosferi. Za procjenu efektivne temperature atmosfere Stefan-Boltzmannovim zakonom korištena je vrijednost solarne konstante izmjerena satelitom Nimbus-7 na kanalu 100. Efekt staklenika definiran je kao razlika između temperature na površini i efektivne temperature atmosfere.
Izračunata je godišnja varijacija intenziteta efekta staklenika, te je nađena logaritmička veza izme|u intenziteta efekta staklenika i količine vodene pare u atmosferi.

Creator (Dublin Core)

Rakoczi, Ferenz

Ivanyi, Zsuzsanna

Subject (Dublin Core)

eng Greenhouse effect; water vapor

hrv efekt staklenika; vodena para

Publisher (Dublin Core)

Andrija Mohorovicic Geophysical Institute

Date (Dublin Core)

1999

Type (Dublin Core)

text

info:eu-repo/semantics/article

info:eu-repo/semantics/publishedVersion

Format (Dublin Core)

application/pdf

Identifier (Dublin Core)

https://hrcak.srce.hr/17671

eng https://hrcak.srce.hr/file/27337

Source (Dublin Core)

Geofizika

ISSN 0352-3659 (Print)

ISSN 1846-6346 (Online)

Volume 16-17

Issue 1

Language (Dublin Core)

eng

Rights (Dublin Core)

info:eu-repo/semantics/openAccess

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