Vízrajzi Évkönyv 99., 1994 (Budapest, 1995)
Tartalomjegyzék
GENERAL INFORMATION 1. The symbols used in this Annual are as follows ”0” L point zero of the water-gauge distance from the estuary NV 1 NV 1 high-water level. The highest gauge reading observed within a given period high-water level in the presence of ice. Highest gauF catchment area ge reading observed in the presence of ice within a ice on the banks given period 1 LKV drifting ice standing ice lowest low-water level. Lowest gauge reading as to LNV IlnvI highest high-water level. The highest gauge reading as to yet recorded highest high-water level in the presence of ice Ilk-yI yet recorded lowest low-water level in the presence of ice. LoKQ low-water discharge. The lowest discharge occurring within a given period west gauge reading recorded as to yet in the presence of ice KKQ mean low-water discharge. Arithmetical mean of low discharges occurring within a given period KV low-water level. Lowest gauge reading recorded within a given period KÖQ mean water discharge. Arithmetical mean of daily discharges occurring within a given period LkyJ low-water level in the presence of ice. Lowest gauge reading in the presence of ice recorded within a giNQ high-water discharge. The highest discharge occurring within a given period ven period 2Q annual total discharge KKV mean low-water level. Arithmental mean of the lowKq \ KQ ] converted to 1km2 value of •{ KÖQ }■ of the catchment waters occurring within a given period KÖq KÖV mean water level. Arithmetical mean of gauge reaNq NOQ J area KNV ding series mean high-water level. Arithmetical mean of highm B. f. elevation above the Baltic level, in waters occuring within a given period- 17-
