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EN
In 2009–2010, in five points in Lublin, located in areas of different land use and built-up, measurements of air temperature and humidity were taken. Based on the data collected, the following elements were calculated: the difference in average monthly air temperature between the coldest point and the others, equivalent temperature (Tek) and Tek thermal sensations. Differencesin average monthly air temperature in relation to the outskirts of Lublin were the highest at the point Dominikanie, in the built-up area of the old town. Most frequently “sultry” sensation was reported for the estate houses, at the point Ofelii. Different biothermal conditions were observed in the center of the city – Litewski square. It is characterized by a high proportion of vegetation. Green areas influenced the reduction of the biothermal stress compared to other points. The highest frequency of thermal sensation “cold”, “cool” and “slightly cool” were recorded there. Measurements points located in two housing estates with high buildings close to each other were characterized by similar biothermal conditions. In these areas, comparing to other discussed areas of the city, at 12 UTC relatively often there were noticed the best biothermal conditions – “comfortable” according to equivalent temperature index.
PL
Artykuł nie zawiera abstraktu w języku polskim
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Zarys bioklimatu Zamościa

48%
Facta Simonidis
|
2023
|
vol. 16
|
issue 1
341-356
EN
The paper uses data from meteorological stations operating in Zamość in the period from 1976 to 2020. The variability of the values of selected meteorological elements and climatic characteristics on a time scale was presented using the most commonly used distribution statistics, i.e. average values and variability measures. The direction of the trend of changes in air temperature was determined as well. In order to determine the bioclimatic conditions, the values of selected indicators were calculated, including equivalent temperature, effective temperature, and air cooling quantity. The conducted research indicates that in Zamość optimal thermal conditions described as pleasantly cool occur in the summer ( June, July, August), while in July they are mild. In April, May and September, the thermal sensation is characterized as cool. Generally, it is cold from November to March and very cold in January and February.
PL
W pracy wykorzystano dane ze stacji meteorologicznych funkcjonujących na terenie Zamościa w okresie od 1976 do 2020 roku. Opisano zmienność wartości wybranych elementów meteorologicznych i charakterystyk klimatycznych w skali czasowej, wykorzystując najczęściej stosowane statystyki rozkładu, tzn. wartości średnie oraz miary zmienności. Wyznaczono kierunek trendu zmian temperatury powietrza. W celu określenia warunków bioklimatycznych obliczono wartości wybranych wskaźników, takich jak: temperatura ekwiwalentna, temperatura efektywna i wielkość ochładzająca powietrza. Przeprowadzone badania wskazują, że w Zamościu optymalne warunki termiczne określane jako przyjemnie chłodno występują w okresie letnim (czerwiec, lipiec, sierpień), przy czym w lipcu są one łagodne. W kwietniu, maju i we wrześniu odczucie cieplne charakteryzowane jest jako chłodne. Generalnie w okresie od listopada do marca jest zimno, a w styczniu i w lutym bardzo zimno.
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