Titlebook: Ross Sea Ecology; Italiantartide Exped Francesco Maria Faranda,Letterio Guglielmo,Adriann Book 2000 Springer-Verlag Berlin Heidelberg 2000

medieval

Climatic Characterization of the Terra Nova Bay Region upper level soundings are also conducted. In the present chapter the climatological data, collected in about a decade, are analyzed to give a climatic picture of Terra Nova Bay. The parameters considered are radiation, pressure, temperature, humidity and wind. The obtained results have been compare

Retrieval

Oxygen Isotope Characterization of Terra Nova Bay Seawaterand evolution of the water masses is discussed by comparing δ.O values with salinity data on δ.O/S diagrams. The mean δ.O values ranged from ?0.33 to ?0.23‰ for AASW and were close to ?0.36‰ for HSSW and ?0.45‰ for ISW.

分貝

Biogeochemical Processes in the Ross Sea (Antarctica): Present Knowledge and Perspectiveson can be explained by post-bloom mechanisms. Sediments at mooring sites, A B and C showed different lithologies, with C representing conditions of no present sediment accumulation. Composition, density and structure of benthic communities also differed significantly, mostly as a function of water d

錢財(cái)

Blood-Clot

pacific

動(dòng)物

fidelity

Spatial and Temporal Patterns of Nutrient Distributions in the Ross Seariation in spatial and temporal nutrient patterns in the Ross Sea, in relation with physical and biological processes. Due to a slower recycling rate of Si compared to the N and P cycles, high Si concentrations and different evolution of the N/P and Si/N ratios are typical of CDW and of that part of

有發(fā)明天才

VICT