Number of days available for climatic review
parametr | sty | lut | mar | kwi | maj | cze |
Tmax | 1066 | 983 | 1084 | 1045 | 1085 | 1055 |
Tmin | 1068 | 982 | 1089 | 1049 | 1085 | 1055 |
słońce (godz.) | 0 | 0 | 0 | 0 | 0 | 0 |
opad | 620 | 560 | 620 | 600 | 620 | 600 |
wilgotność / widzialność | 0 | 0 | 0 | 0 | 0 | 0 |
parametr | lip | sie | wrz | paź | lis | gru |
Tmax | 1101 | 1101 | 1059 | 1128 | 1083 | 1104 |
Tmin | 1102 | 1101 | 1066 | 1126 | 1084 | 1105 |
słońce (godz.) | 0 | 0 | 0 | 0 | 0 | 0 |
opad | 620 | 620 | 600 | 620 | 600 | 620 |
wilgotność / widzialność | 0 | 0 | 0 | 0 | 0 | 0 |
Climate data is usually derived from meteorological data of a certain number of years. The actual number of recorded years may vary from only a couple to 50 years or more. The quality of climate data depends on the number of available recorded years. Fewer years means less reliable data. The standart-period for reliable climate data is 30 years. For example, the mean monthly temperature for, let's say January, would ideally calculated from a total number of 930 recorded January-days. However, the usual number of recorded days is much smaller. The table above shows the actual number of recorded days for every parameter measured. |