By Peter Knight
Glacier technology and Environmental swap is a accomplished reference paintings studying modern matters in glaciology and explores the interface among glacier technology and environmental swap, prior, current, and destiny.
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Extra resources for Glacier Science and Environmental Change
Example text
Erosional marks on Kellys Island, Lake Erie (c, photograph by Mandy Munro-Stasiuk). These erosional marks show the integration of crescentic scour and linear furrows and several identical elements appear in (a) and (c), particularly hairpin scours and the way in which crescentic scours define the pointed, proximal parts of rock drumlins. 1 Streamlined hills Streamlined hills in Antarctica are up to 300 m high and they are aligned with subglacial meltwater flow rather than ice flow (Sawagaki & Hirakawa, 1997).
2005b). The gradient of the SSC versus Q graph (Fig. 3) is determined by the relationship between the sedimenttransporting capacity of the flow, which scales linearly with flow velocity, and discharge. 3 under predominantly distributed subglacial drainage conditions. 2 under flow predominantly through hydraulically efficient channels. , 2005a,b). Relationship intercepts (Fig. 3) demonstrate changes in sediment availability under both distributed and channelized conditions, most notably a relative increase in availability between subperiods 5 and 8.
Notably, the efficiency of sediment evacuation appeared to be lowest during subperiod 5 (Fig. , 2005a) and reached a maximum during subperiod 8 (Fig. 2d) when up-glacier extension of the network had largely ceased. Relationships between SSC and Q (Fig. 3) for shorter periods of the melt season (cf. Fig. , 2005b). The gradient of the SSC versus Q graph (Fig. 3) is determined by the relationship between the sedimenttransporting capacity of the flow, which scales linearly with flow velocity, and discharge.
