The main features of the hydrological regime and morphological structure of the estuarine-type mo... more The main features of the hydrological regime and morphological structure of the estuarine-type mouth area of the Saint Lawrence River are considered. Data on the structure of water masses, thermal and ice regimes in the Gulf of Saint Lawrence, which has a significant effect on the estuary, are given. The major attention is paid to water mixing processes, water and sediment dynamics in the estuary under the joint effect of river runoff and tides, and as a function of bed topography. The parameter determining the type of water stratification and circulation is discussed. The effect of the Coriolis force on the stratified flow in the estuary and formation of the geostrophic current is discussed.
... QIV Kazanskaya vein QIV Utesnoe Pustoe Olen'ino Bokontya QIV 0 4 km 132°00′ ... Heav... more ... QIV Kazanskaya vein QIV Utesnoe Pustoe Olen'ino Bokontya QIV 0 4 km 132°00′ ... Heavy concentrate sampling in the interfluve of the Uga khan–Utesnaya aureole (23 km2) was discovered in the area of right tributaries of the Ugakhan River and Utesnaya stream basin. ...
The characteristics of rain and point charges based on routine measurements extending over four r... more The characteristics of rain and point charges based on routine measurements extending over four rainy seasons are presented. An average rain current density of (1.0±0.1)×10−10 A m−2 and charge per unit volume of rain water of (0.43±0.02)×10−4 C m−3 for the locality are obtained, which are compared with data obtained elsewhere by other workers. The point-discharge current measurements lead to a revised estimate of (0.86±0.08)×10−9 A m−2 for the average point discharge current below storm clouds.
The main features of the hydrological regime and morphological structure of the estuarine-type mo... more The main features of the hydrological regime and morphological structure of the estuarine-type mouth area of the Saint Lawrence River are considered. Data on the structure of water masses, thermal and ice regimes in the Gulf of Saint Lawrence, which has a significant effect on the estuary, are given. The major attention is paid to water mixing processes, water and sediment dynamics in the estuary under the joint effect of river runoff and tides, and as a function of bed topography. The parameter determining the type of water stratification and circulation is discussed. The effect of the Coriolis force on the stratified flow in the estuary and formation of the geostrophic current is discussed.
... QIV Kazanskaya vein QIV Utesnoe Pustoe Olen'ino Bokontya QIV 0 4 km 132°00′ ... Heav... more ... QIV Kazanskaya vein QIV Utesnoe Pustoe Olen'ino Bokontya QIV 0 4 km 132°00′ ... Heavy concentrate sampling in the interfluve of the Uga khan–Utesnaya aureole (23 km2) was discovered in the area of right tributaries of the Ugakhan River and Utesnaya stream basin. ...
The characteristics of rain and point charges based on routine measurements extending over four r... more The characteristics of rain and point charges based on routine measurements extending over four rainy seasons are presented. An average rain current density of (1.0±0.1)×10−10 A m−2 and charge per unit volume of rain water of (0.43±0.02)×10−4 C m−3 for the locality are obtained, which are compared with data obtained elsewhere by other workers. The point-discharge current measurements lead to a revised estimate of (0.86±0.08)×10−9 A m−2 for the average point discharge current below storm clouds.
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