. "Microclimate of tourist attractive areas of Brno city"@en . . "S" . . . . . "Pomoc\u00ED stacion\u00E1rn\u00EDho m\u011B\u0159en\u00ED teploty vzduchu nad asfaltov\u00FDm povrchem, m\u011B\u0159en\u00ED teplot povrch\u016F a p\u0159ilehl\u00E9 vzduchov\u00E9 vrstvy mobiln\u00EDm monitoringem a bezkontaktn\u00EDho m\u011B\u0159en\u00ED teploty povrch\u016F pomoc\u00ED termovizn\u00ED kamery byl monitorov\u00E1n tepeln\u00FD ostrov m\u011Bsta Brna. Zvl\u00E1\u0161tn\u00ED pozornost byla v\u011Bnov\u00E1na dn\u016Fm s vysokou teplotou vzduchu (tropick\u00FDm dn\u016Fm) a vysokou hodnotou glob\u00E1ln\u00ED radiace, kdy je p\u0159edpokl\u00E1d\u00E1n nejvy\u0161\u0161\u00ED vliv atropogenn\u00EDch povrch\u016F na teplotu vzduchu. Byl potvrzen v\u00FDrazn\u00FD vliv tmav\u00E9ho povrchu na stratifikaci teplot ve vertik\u00E1ln\u00EDm profilu zejm\u00E9na cca od 9:00 do 20:00, kter\u00FD koresponduje s intenzitou p\u0159\u00EDkonu sol\u00E1rn\u00ED radiace. Maxim\u00E1ln\u00ED rozd\u00EDly %22p\u0159\u00EDzemn\u00ED%22 teploty vzduchu a teploty ve 2 nad povrchem se pohybuj\u00ED okolo 3 \u00B0C a byly zaznamen\u00E1ny okolo 15. hodiny. V tmav\u00E9 \u010D\u00E1sti dne se diference b\u011Bhem kr\u00E1tk\u00E9 doby vyrovnaj\u00ED a dosahuj\u00ED maxim\u00E1ln\u011B okolo 1 \u00B0C. B\u011Bhem mobiln\u00EDho monitoringu v nejnav\u0161t\u011Bvovan\u011Bj\u0161\u00EDch \u010D\u00E1stech Brna byly zji\u0161t\u011Bny diference povrchov\u00E9 teploty materi\u00E1l\u016F na \u00FArovni a\u017E 25 \u00B0C (voda, travn\u00ED porost, d\u0159evo, p\u00EDsek, beton, asfalt, kov, etc.). Rozd\u00EDl mezi teplotou vzduchu a teploty povrch\u016F \u010Dinil a\u017E 27,4 \u00B0C (vzduch versus asfalt). P\u0159i pou\u017Eit\u00ED termovizn\u00ED kamery vz\u00E1jemn\u00E9 porovn\u00E1n\u00ED identick\u00FDch ploch ukazuje, \u017Ee teplota povrchu se u zastav\u011Bn\u00FDch ploch zv\u00FD\u0161ila za t\u0159i hodiny o cca 10 \u00B0C, p\u0159i\u010Dem\u017E teploty povrch\u016F dosahovaly i 50 \u00B0C. Zazelen\u011Bn\u00E9 plochy vykazuj\u00ED podstatn\u011B ni\u017E\u0161\u00ED n\u00E1r\u016Fst teplot a pohybuje se na \u00FArovni n\u00E1r\u016Fstu teploty vzduchu tj. o cca 3 \u00B0C, p\u0159i\u010Dem\u017E maxim\u00E1ln\u00ED teploty se pohybovali na \u00FArovni 34\u00B0C. Rozd\u00EDl teploty povrch\u016F zastav\u011Bn\u00FDch ploch s plochami osazen\u00FDmi zelen\u00ED jsou t\u00E9m\u011B\u0159 20\u00B0C. Z porovn\u00E1n\u00ED v\u00FDsledk\u016F je jasn\u011B vid\u011Bt funkci zelen\u011B, kter\u00E9 dok\u00E1\u017Ee d\u00EDky v\u00FDpar\u016Fm vody podstatn\u011B l\u00E9pe odv\u00E1d\u011Bt teplo z dopadaj\u00EDc\u00EDho slune\u010Dn\u00EDho z\u00E1\u0159en\u00ED ne\u017E je tomu u stavebn\u00EDch objekt\u016F." . "A heat island of Brno city was monitored by stationary measurements of air temperature above the asphalt surface, by surface and adjacent air layer temperature measurements and by mobile contactless surface temperature measurement using thermal camera. Particular attention was paid to the days with a high air temperature (tropical days) and a high value of global radiation when the highest anthropogenic impact of anthropogenic surfaces on air temperature is expected. A significant effect of a dark surface on temperature stratification in vertical profile especially around 9:00 to 8:00 p.m. was confirmed. It corresponds to the solar radiation intensity. The maximum difference of a %22ground%22 temperature and air temperature at 2 m above the surface reached to 3\u00B0C and were observed at about 3:00 p.m. The difference of dark part of the day fast diminish and reaches maximum 1\u00B0C.Thermal monitoring of tourist the most popular parts of Brno detected about 25\u00B0C differences of surface temperature of different materials (water, grassland, timber, sand, concrete, asphalt, metal, etc.). The differences of air temperature and surface temperature reached to 27.4\u00B0C (air versus asphalt). Comparison of identic areas in different daily time by thermal camera images shows that surface temperatures in built-up areas increased during three hours about 10\u00B0C, (the surface temperatures reached even 50\u00B0C). The areas with vegetation embody a significantly lower temperature increase (i.e. about 3\u00B0C with maximum temperature of 34\u00B0C). The surface temperature differences of built-up areas and areas with vegetation reached to 20\u00B0C. The comparison of the results showed a vegetation influence on temperature regulation due to vapour."@en . "978-80-7375-507-2" . . . "Pomoc\u00ED stacion\u00E1rn\u00EDho m\u011B\u0159en\u00ED teploty vzduchu nad asfaltov\u00FDm povrchem, m\u011B\u0159en\u00ED teplot povrch\u016F a p\u0159ilehl\u00E9 vzduchov\u00E9 vrstvy mobiln\u00EDm monitoringem a bezkontaktn\u00EDho m\u011B\u0159en\u00ED teploty povrch\u016F pomoc\u00ED termovizn\u00ED kamery byl monitorov\u00E1n tepeln\u00FD ostrov m\u011Bsta Brna. Zvl\u00E1\u0161tn\u00ED pozornost byla v\u011Bnov\u00E1na dn\u016Fm s vysokou teplotou vzduchu (tropick\u00FDm dn\u016Fm) a vysokou hodnotou glob\u00E1ln\u00ED radiace, kdy je p\u0159edpokl\u00E1d\u00E1n nejvy\u0161\u0161\u00ED vliv atropogenn\u00EDch povrch\u016F na teplotu vzduchu. Byl potvrzen v\u00FDrazn\u00FD vliv tmav\u00E9ho povrchu na stratifikaci teplot ve vertik\u00E1ln\u00EDm profilu zejm\u00E9na cca od 9:00 do 20:00, kter\u00FD koresponduje s intenzitou p\u0159\u00EDkonu sol\u00E1rn\u00ED radiace. Maxim\u00E1ln\u00ED rozd\u00EDly %22p\u0159\u00EDzemn\u00ED%22 teploty vzduchu a teploty ve 2 nad povrchem se pohybuj\u00ED okolo 3 \u00B0C a byly zaznamen\u00E1ny okolo 15. hodiny. V tmav\u00E9 \u010D\u00E1sti dne se diference b\u011Bhem kr\u00E1tk\u00E9 doby vyrovnaj\u00ED a dosahuj\u00ED maxim\u00E1ln\u011B okolo 1 \u00B0C. B\u011Bhem mobiln\u00EDho monitoringu v nejnav\u0161t\u011Bvovan\u011Bj\u0161\u00EDch \u010D\u00E1stech Brna byly zji\u0161t\u011Bny diference povrchov\u00E9 teploty materi\u00E1l\u016F na \u00FArovni a\u017E 25 \u00B0C (voda, travn\u00ED porost, d\u0159evo, p\u00EDsek, beton, asfalt, kov, etc.). Rozd\u00EDl mezi teplotou vzduchu a teploty povrch\u016F \u010Dinil a\u017E 27,4 \u00B0C (vzduch versus asfalt). P\u0159i pou\u017Eit\u00ED termovizn\u00ED kamery vz\u00E1jemn\u00E9 porovn\u00E1n\u00ED identick\u00FDch ploch ukazuje, \u017Ee teplota povrchu se u zastav\u011Bn\u00FDch ploch zv\u00FD\u0161ila za t\u0159i hodiny o cca 10 \u00B0C, p\u0159i\u010Dem\u017E teploty povrch\u016F dosahovaly i 50 \u00B0C. Zazelen\u011Bn\u00E9 plochy vykazuj\u00ED podstatn\u011B ni\u017E\u0161\u00ED n\u00E1r\u016Fst teplot a pohybuje se na \u00FArovni n\u00E1r\u016Fstu teploty vzduchu tj. o cca 3 \u00B0C, p\u0159i\u010Dem\u017E maxim\u00E1ln\u00ED teploty se pohybovali na \u00FArovni 34\u00B0C. Rozd\u00EDl teploty povrch\u016F zastav\u011Bn\u00FDch ploch s plochami osazen\u00FDmi zelen\u00ED jsou t\u00E9m\u011B\u0159 20\u00B0C. Z porovn\u00E1n\u00ED v\u00FDsledk\u016F je jasn\u011B vid\u011Bt funkci zelen\u011B, kter\u00E9 dok\u00E1\u017Ee d\u00EDky v\u00FDpar\u016Fm vody podstatn\u011B l\u00E9pe odv\u00E1d\u011Bt teplo z dopadaj\u00EDc\u00EDho slune\u010Dn\u00EDho z\u00E1\u0159en\u00ED ne\u017E je tomu u stavebn\u00EDch objekt\u016F."@cs . . "St\u0159edov\u00E1, Hana" . . "Mikroklima turisticky nav\u0161t\u011Bvovan\u00FDch \u010D\u00E1st\u00ED m\u011Bsta na p\u0159\u00EDkladu Brna" . "320756900014" . "[13DD3F4EFBA5]" . "RIV/62156489:43210/11:00170749" . "Ro\u017Enovsk\u00FD, Jaroslav" . "212478" . . "Mikroklima turisticky nav\u0161t\u011Bvovan\u00FDch \u010D\u00E1st\u00ED m\u011Bsta na p\u0159\u00EDkladu Brna" . "2011-05-04+02:00"^^ . "Mikroklima turisticky nav\u0161t\u011Bvovan\u00FDch \u010D\u00E1st\u00ED m\u011Bsta na p\u0159\u00EDkladu Brna"@cs . "RIV/62156489:43210/11:00170749!RIV13-MSM-43210___" . . "St\u0159eda, Tom\u00E1\u0161" . "Microclimate of tourist attractive areas of Brno city"@en . . . "7"^^ . "MENDELU v Brn\u011B" . "Urban heat island; temperature monitoring"@en . "43210" . . "3"^^ . "Mikroklima turisticky nav\u0161t\u011Bvovan\u00FDch \u010D\u00E1st\u00ED m\u011Bsta na p\u0159\u00EDkladu Brna"@cs . "Brno" . "Public recreation and landscape protection - hand in hand?" . "Brno" . "3"^^ . . .