Construct · 1 fields · 1 citations

tidewater glacier cycle: a standalone construct

One name. One construct. A landmark on the map.

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Sea-level and cryosphere science

the slow advance and rapid, partly climate-independent retreat of calving glaciers controlled by water depth at the terminus.

In sea-level and cryosphere science, tidewater glacier cycle refers to the slow advance and rapid, partly climate-independent retreat of calving glaciers controlled by water depth at the terminus. This meaning comes from Meier (1987) in Journal of Geophysical Research: Solid Earth.[1]

Unit
Recovery means
Measured by

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Nearby constructs

calving1 fields · 1 citationsanchor · a standalone construct cycle4 fields · 4 citationsjingle · one word, four constructs depth3 fields · 6 citationsjingle · one word, three constructs

References

Meier, M. F., & Post, A. (1987). Fast tidewater glaciers. Journal of Geophysical Research: Solid Earth, 92(B9), 9051-9058. https://doi.org/10.1029/jb092ib09p09051

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