Vízrajzi Évkönyv 88., 1983 (Budapest, 1984)
Tartalomjegyzék
GENERAL INFORMATION 1. The symbols used in this Annual are as follows: F (286) 25- 560 + 26: 52 i 401 LKV iLKVl point zero of the water-gauge warning referring to the fact that the zero point water-gauge has been changed since the year 1931. catchment area value deduced from observation data annual minimum annual maximum ice on the banks drifting ice standing ice lowest low - water level. Lotvest gauge reading as to yet recorded. lowest low-water level in the presence of ice. Lowest gauge reading recorded as to yet in the presence of ice. NV high - water level. The highest gauge reading observed within a given period. 1NVI high-water level in the presence of ice. Highest gauge reading observed in the presence of ice within a given period. LNV highest high-water level. The highest gauge reading as to yet recorded. lLNVl highest high-water level in the presence of ice. KQ low-water discharge. The lowest discharge occurring within a given period. KKQ mean low-water discharge. Arithmetical mean of low discharges occurring within a given period. KÓQ mean water discharge. Arithmetical mean of daily discharges occurring within a given period. KNQ mean high-water discharge. Arithmetical mean of high discharges occurring within a given period. KV low-water level. Lowest gauge reading [KVJ recorded within a given period. NQ high-water discharge. The highest discharge occurring within a given period. low-water level in the presence of ice. Lowest gauge reading in the presence ZQ annual total discharge of ice recorded within a given period. KKV mean low - water level. Arithmetical Kq KQ converted to 1 km mean of the low-waters occurring within a given period. KÖq value of * KÖQ ’ of the catchment Nq NQ area KÖV mean water level. Arithmetical mean of gauge reading series. m B. f. elevation above the Baltic level, m KN V mean high - water level. Arithmetical mean of high-water occurring within a given period.-21 -
