Vízrajzi Évkönyv 96., 1991 (Budapest, 1992)
Tartalomjegyzék
GENERAL INFORMATION 1. The symbols used in this Annual are as follows: "0" point zero of the water-gauge |NV| high-water level in the presence of ice. L distance from the estuary Highest gauge reading observed in the presence of ice within a given period F catchment area LNV highest high-water level. The highest gauge ice on the banks reading as to yet recorded drifting ice |LNV| highest high-water level in the presence of 1 standing ice ice LKV lowest low-water level. Lowest gauge reading as to yet recorded KQ low-water discharge. The lowest discharge occurring within a given period |LKV| lowest low-water level in the presence of ice. Lowest 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. I.owest gauge reading recorded within a given period KÖQ mean water discharge. Arithmetical mean of daily discharges occurring within a given period JKVi low-water level in the presence of ice. Lowest gauge reading in the presence of ice recorded within a given period NQ high-water discharge. The highest discharge occurring within a given period KKV mean low-water level. Arithmetical mean of XQ annual total discharge KÖV the low-water occurring within a given period Kq KÖq 2 f KQ ] converted to 1 km value of ] KÖQ f of the catchment mean water level. Arithmetical mean of gauge reading series Nq 1 NQ J area m B.f. elevation above the Baltic level, m KNV mean high-water level. Arithmetical mean of high-water occurring within a given period NV high - water level. The highest gauge reading observed within a given period- 17-
