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- W4312205053 endingPage "978" @default.
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- W4312205053 abstract "Abstract Initially a matter of intellectual curiosity, but now important for understanding ice‐sheet dynamics, the formation of subglacial bedforms has been a subject of scientific enquiry for over a century. Here, we use a numerical model of the coupled flow of ice, water, and subglacial sediment to explore the formation of subglacial ribs (i.e., ribbed moraine), drumlins and mega‐scale glacial lineations (MSGLs). The model produces instabilities at the ice–bed interface, which result in landforms resembling subglacial ribs and drumlins. We find that a behavioural trajectory is present. Initially subglacial ribs form, which can either develop into fields of organized drumlins, or herringbone‐type structures misaligned with ice flow. We present potential examples of these misaligned bedforms in deglaciated landscapes, the presence of which means caution should be taken when interpreting cross‐cutting bedforms to reconstruct ice flow directions. Under unvarying ice flow parameters, MSGLs failed to appear in our experiments. However, drumlin fields can elongate into MSGLs in our model if low ice–bed coupling conditions are imposed. The conditions under which drumlins elongate into MSGLs are analogous to those found beneath contemporary ice streams, providing the first mechanism, rather than just an association, for linking MSGLs with ice stream flow. We conclude that the instability theory, as realized in this numerical model, is sufficient to explain the fundamental mechanics and process‐interactions that lead to the initiation of subglacial bedforms, the development of the distinctive types of bedform patterns, and their evolutionary trajectories. We therefore suggest that the first part of the longstanding ‘drumlin problem’ – how and why they come into existence – is now solved. However, much remains to be discovered regarding the exact sedimentary and hydrological processes involved." @default.
- W4312205053 created "2023-01-04" @default.
- W4312205053 creator A5034096161 @default.
- W4312205053 creator A5064341140 @default.
- W4312205053 creator A5079622706 @default.
- W4312205053 creator A5080808099 @default.
- W4312205053 date "2023-01-20" @default.
- W4312205053 modified "2023-09-25" @default.
- W4312205053 title "Numerical modelling of subglacial ribs, drumlins, herringbones, and mega‐scale glacial lineations reveals their developmental trajectories and transitions" @default.
- W4312205053 cites W1499331858 @default.
- W4312205053 cites W1560634373 @default.
- W4312205053 cites W1569211986 @default.
- W4312205053 cites W1622283437 @default.
- W4312205053 cites W1675540088 @default.
- W4312205053 cites W1676905481 @default.
- W4312205053 cites W1882258977 @default.
- W4312205053 cites W1885588137 @default.
- W4312205053 cites W1949130384 @default.
- W4312205053 cites W1965233876 @default.
- W4312205053 cites W1967056015 @default.
- W4312205053 cites W1968637371 @default.
- W4312205053 cites W1970086177 @default.
- W4312205053 cites W1972832574 @default.
- W4312205053 cites W1972924623 @default.
- W4312205053 cites W1973402039 @default.
- W4312205053 cites W1973535125 @default.
- W4312205053 cites W1974531601 @default.
- W4312205053 cites W1974711244 @default.
- W4312205053 cites W1975900719 @default.
- W4312205053 cites W1976043511 @default.
- W4312205053 cites W1976193030 @default.
- W4312205053 cites W1979813018 @default.
- W4312205053 cites W1980661496 @default.
- W4312205053 cites W1980688843 @default.
- W4312205053 cites W198461670 @default.
- W4312205053 cites W1986344849 @default.
- W4312205053 cites W1988842878 @default.
- W4312205053 cites W1988867676 @default.
- W4312205053 cites W1989920231 @default.
- W4312205053 cites W1996797557 @default.
- W4312205053 cites W1998131265 @default.
- W4312205053 cites W2001962910 @default.
- W4312205053 cites W2004551162 @default.
- W4312205053 cites W2004716724 @default.
- W4312205053 cites W2006160905 @default.
- W4312205053 cites W2009181711 @default.
- W4312205053 cites W2011923336 @default.
- W4312205053 cites W2013273491 @default.
- W4312205053 cites W2015211281 @default.
- W4312205053 cites W2015993658 @default.
- W4312205053 cites W2019979254 @default.
- W4312205053 cites W2020440388 @default.
- W4312205053 cites W2021593506 @default.
- W4312205053 cites W2025974180 @default.
- W4312205053 cites W2027650088 @default.
- W4312205053 cites W2028322100 @default.
- W4312205053 cites W2029247266 @default.
- W4312205053 cites W2029486441 @default.
- W4312205053 cites W2046473527 @default.
- W4312205053 cites W2054754818 @default.
- W4312205053 cites W2055658052 @default.
- W4312205053 cites W2056421521 @default.
- W4312205053 cites W2058218337 @default.
- W4312205053 cites W2059021524 @default.
- W4312205053 cites W2066983326 @default.
- W4312205053 cites W2067413684 @default.
- W4312205053 cites W2069580113 @default.
- W4312205053 cites W2070901304 @default.
- W4312205053 cites W2074045925 @default.
- W4312205053 cites W2074832795 @default.
- W4312205053 cites W2078811681 @default.
- W4312205053 cites W2080603294 @default.
- W4312205053 cites W2089069372 @default.
- W4312205053 cites W2090723086 @default.
- W4312205053 cites W2099093517 @default.
- W4312205053 cites W2103629802 @default.
- W4312205053 cites W2108611747 @default.
- W4312205053 cites W2109110585 @default.
- W4312205053 cites W2109451901 @default.
- W4312205053 cites W2112184582 @default.
- W4312205053 cites W2113159671 @default.
- W4312205053 cites W2117168188 @default.
- W4312205053 cites W2118183473 @default.
- W4312205053 cites W2121718829 @default.
- W4312205053 cites W2128455066 @default.
- W4312205053 cites W2137729488 @default.
- W4312205053 cites W2137952547 @default.
- W4312205053 cites W2141597491 @default.
- W4312205053 cites W2146989730 @default.
- W4312205053 cites W2147696707 @default.
- W4312205053 cites W2149061491 @default.
- W4312205053 cites W2161286215 @default.
- W4312205053 cites W2165287893 @default.
- W4312205053 cites W2167118049 @default.
- W4312205053 cites W2176369079 @default.
- W4312205053 cites W2229014138 @default.
- W4312205053 cites W2260747293 @default.
- W4312205053 cites W2285277585 @default.