首页 | 本学科首页   官方微博 | 高级检索  
     检索      


A contribution to the parameterization of total radiation
Authors:Jan Pretel  Lilian Kir?nerová  Reviewer K Vaní?ek
Institution:(1) Institute of the Physics of the Atmosphere, Czechosl. Acad. Sci., Prague
Abstract:Summary To be able to parameterize vertical heat and water vapour fluxes in the boundary layer of the atmosphere, it is necessary to determined, among other factors, the amount of incident total radiation under a generally arbitrary condition of the atmosphere at any instant of time. This paper deals with a simple model for computing the total radiation based on known solar elevation, total cloud cover and the atmospheric turbidity parameter. This variant of the model was formulated on the basis of a two-year series of total radiation observations made in the radiation network of the Czech Hydrometeorological Institute, and on the measurements and observations made at the observatory of the Institute of the Physics of the Atmosphere in Kopisty. An example of comparing the observed and theoretical values of total radiation will also be given.
Rcyiecyzcyyucymcyiecy Ncyiecyocybcykhcyocy¶rt;umcyocyscymsoftcy narcyamcyiecymrcyuzcyatscyuu vcyiecyrcymukcyalcysoftcyncyycykhcy nocymocykcyocyvcy miecynlcya u vcylcyazhcyncyocyscymu vcy nocyzrcyancyuchcyncyocymcy scylcyocyiecy ammcyocyscyfcyiecyrcyycy mrcyiecybcyucyiecym mcyiecyzhcy¶rt;ucy nrcyocychcyumcy ocynrcyiecy¶rt;iecylcyiecyncyuiecy zcyncyachcyiecyncyuyacy ncya zcyiecymcyncyucyyucy nocyvcyiecyrcykhcyncyocyscymsoftcy nrcyumiecykcyayucyshchcyiecyubreve scyucymcymcyarcyncyocyubreve rcya¶rt;uatscyuu vcy lcyyucybcyocyubreve mcyocymcyiecyncym vcyrcyiecymcyiecyncyu. Scymamsoftcyyacy zcyancyumcyaiecymscyyacy vcyocynrcyocyscyocymcy ocy narcyamcyiecymrcyuzcyatscyuu scyucymcymcyarcyncyocyubreve rcya¶rt;uatscyuu nocy ¶rt;ancyncyycymcy ocy vcyycyscyocymiecy Scyocylcyncytscya, zcyamcyucymncyiecyncyncyocyscymu ammcyocyscyfcyiecyrcyycy u scymiecyniecyncyu ocybcylcyachcyncyocyzocy nocykcyrcyycyvcya. Pcyrcyiecy¶rt;lcyazaiecymcyayacy mcyocy¶rt;iecylcysoftcy nocyscymrcyocyiecyncya ncya ocyscyncyocyvcyiecy rcyiecyzcyucylcysoftcymamocyvcy ¶rt;vcyucykhcylcyiecymncyukhcy uzcymcyiecyrcyiecyncyuubreve vcy rcyatscyuatscyuocyncyncyocyubreve scyiecymu CHcyiecyshcyscykcyocyzocy zu¶rt;rcyocymcyiecymiecyocyrcyocylcyocyzuchcyiecyscy kcyocyzocy uncyscymumucyma u ncya ocybcyscyiecyrcyvcyamocyrcyuu Icyncyscymumucyma fcyuzcyukcyu ammcyocyscyfcyiecyrcyycy AcyNcy CHcyScyScyRcy vcy Kcyocynuscymakhcy. Vcy scymamsoftcyiecy makcyzhcyiecy nrcyuvcyiecy¶rt;iecyncy nrcyumcyiecyrcy scyrcyavcyncyiecyncyuyacy uzcymcyiecyrcyiecyncyncyycykhcy u nocy nrcyiecy¶rt;lcyocyzhcyiecyncyncyocyubreve mcyocy¶rt;iecylcyu vcyycychcyuscylcyiecyncyncyycykhcy zcyncyachcyiecyncyuubreve scyucymcymcyarcyncyocyubreve rcya¶rt;uatscyuu.
Keywords:
本文献已被 SpringerLink 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号