Titlebook: Oceanography of a Large-Scale Estuarine System; The St. Lawrence Mohammed I. El-Sabh,Norman Silverberg Book 1990 Springer Science+Business

因無(wú)茶而冷淡

Fronts and Mesoscale Features in the St. Lawrence Estuary,The influence of freshwater input, wind forcing and tidal processes on the distribution of temperature, salinity and current fields are discussed. Mechanisms responsible for variability of frontal phenomena, eddy formation and coastal jet dynamics are considered as a function of seasonal changes in

N斯巴達(dá)人

來(lái)自于

Recent Sediments and Sediment Transport Processes in the St. Lawrence Estuary,y of the St. Lawrence Upper and Lower Estuaries. On the channel floor, ice contact facies overlain by post-glacial transgressive (Goldthwait) muds form two distinct stratigraphic units under gravel and sand lag deposits, and contemporaneous estuarine silty clays. The upper region is mostly shallow (

OMIT

Nearshore Sediment Dynamics in the St. Lawrence Estuary,400 km long, 70 km wide near the mouth and 15 km wide at the upper end. The dimensions of the Estuary are such that the hydrodynamic conditions prevailing in the lower portion are typically marine while those prevailing in the upper portion are typically estuarine. The tide is semi-diurnal and reach

AUGUR

Arbitrary

好開(kāi)玩笑

Sediment-Water Interaction and Early Diagenesis in the Laurentian Trough,review is made of the role of organic matter (input to the sediment surface, inmixing through bioturbation, degradation by bacteria) and of the distributions of oxidants, nutrients, trace metals and other chemical substances either directly and indirectly involved in the cycling of organic matter. M

RENAL

hematuria

chemical-peel