Absolute moisture content in mid-latitude urban canopy layer, part 2 results from Szeged, Hungary /
This study gives a comprehensive picture on the air humidity observation and mapping in urban canopy layer in Szeged, Hungary, analyzing three-year long vapor pressure dataset (e) calculated from observations of a 22-station urban network. The analysis was divided into two directions, namely the urb...
Elmentve itt :
| Szerzők: | |
|---|---|
| Dokumentumtípus: | Cikk |
| Megjelent: |
2018
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| Sorozat: | Acta climatologica
51-52 |
| Kulcsszavak: | Éghajlattan - nedvességtartalom |
| Tárgyszavak: | |
| doi: | 10.14232/acta.clim.2018. 52 . 3 |
| Online Access: | http://acta.bibl.u-szeged.hu/56833 |
| LEADER | 02339nab a2200253 i 4500 | ||
|---|---|---|---|
| 001 | acta56833 | ||
| 005 | 20220511140050.0 | ||
| 008 | 181217s2018 hu o 0|| eng d | ||
| 022 | |a 563-0614 | ||
| 024 | 7 | |a 10.14232/acta.clim.2018. 52 . 3 |2 doi | |
| 040 | |a SZTE Egyetemi Kiadványok Repozitórium |b hun | ||
| 041 | |a eng | ||
| 100 | 1 | |a Unger János | |
| 245 | 1 | 0 | |a Absolute moisture content in mid-latitude urban canopy layer, part 2 |h [elektronikus dokumentum] : |b results from Szeged, Hungary / |c Unger János |
| 260 | |c 2018 | ||
| 300 | |a 47-56 | ||
| 490 | 0 | |a Acta climatologica |v 51-52 | |
| 520 | 3 | |a This study gives a comprehensive picture on the air humidity observation and mapping in urban canopy layer in Szeged, Hungary, analyzing three-year long vapor pressure dataset (e) calculated from observations of a 22-station urban network. The analysis was divided into two directions, namely the urban-rural and intra-urban ones where the latter was partly based on the local climate zone approach. (i) The general features of the annual and diurnal variations of urban-rural absolute humidity difference in cities with mid-latitude climates are also detectable in the case of Szeged. (ii) In the annual and seasonal e means there is no clear zone sequence that would follow the differences in the compactness or building height of the zones and even the built-up versus land cover distinction. (iii) The highest e values and their differences among stations appear in summer, while the lowest ones in winter and the values of transitional seasons are between them. In certain cases the intra-zone differences can exceed the inter-zone ones since the effect of microscale environment is essential. The decisive factors are the per meability of the surface and the vegetation cover. (iv) The diurnal course of the e pattern in normalized 4-hour time steps does not show a regular shape, the patterns are mosaic-like: in all time steps the driest and wettest areas are mainly in the north-western and south-eastern parts, respectively. | |
| 650 | 4 | |a Természettudományok | |
| 650 | 4 | |a Föld- és kapcsolódó környezettudományok | |
| 695 | |a Éghajlattan - nedvességtartalom | ||
| 700 | 0 | 1 | |a Skarbit N. |e aut |
| 700 | 0 | 1 | |a Gál Tamás |e aut |
| 856 | 4 | 0 | |u http://acta.bibl.u-szeged.hu/56833/1/climatologia_051-052_047-056.pdf |z Dokumentum-elérés |