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Seasonal melt ponding and penetrating under glaciers shows seasonal acceleration and deceleration of ice flows affecting whole icesheets. [ 3 ] Some glaciers experience glacial quakes —glaciers "as large as Manhattan and as tall as the Empire State Building , can move 10 meters in less than a minute, a jolt that is sufficient to generate ...
Under the application of sustained force ice will flow as a fluid, and changes to the force applied will result in non-linear changes to the resulting flow. [4] This fluid behavior of ice, which the Glen–Nye flow law is intended to represent, is accommodated within the solid ice by creep, [4] and is a dominant mode of glacial ice flow. [5] [3 ...
Antarctic ice cores contain trapped air bubbles whose ratios of different oxygen isotopes are a reliable proxy for global temperatures around the time the ice was formed. Study of this data concluded that the climatic response documented in the ice cores was driven by northern hemisphere insolation as proposed by the Milankovitch hypothesis. [ 19 ]
For internal flows, flow separation produces an increase in the flow losses, and stall-type phenomena such as compressor surge, both undesirable phenomena. [8] Another effect of boundary layer separation is regular shedding vortices, known as a Kármán vortex street. Vortices shed from the bluff downstream surface of a structure at a frequency ...
Application of the model to Bering Glacier in Alaska demonstrated a close agreement with ice volume loss for the 1972–2003 period measured with the geodetic method. Determining the mass balance and runoff of the partially debris-covered Langtang Glacier in Nepal demonstrates an application of this model to a glacier in the Himalayan Range. [36]
Ice freezing or melting (Sea ice freezing or melting, ice shelf melting, iceberg melting) Groundwater discharge whereby the 1., 3. and 5. are all inputs, adding freshwater to the ocean, while 2. is an output, i.e. a negative freshwater flux and 4. can be either a freshwater loss (freezing) or gain (melting).
In the summer, glacial streams experience high stream flow because of ice melt. [8] The high flow is characterized by high turbidity and sediment transport, which reduces the biomass of the resident periphyton. [8] At the end of summer, ice melt is reduced and stream flow decreases, causing an increase in the periphyton population. [8]
Runoff is the flow of water across the earth, and is a major component in the hydrological cycle. Runoff that flows over land before reaching a watercourse is referred to as surface runoff or overland flow. Once in a watercourse, runoff is referred to as streamflow, channel runoff, or river runoff. Urban runoff is surface runoff created by ...