2016
DOI: 10.1016/j.csr.2016.01.012
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Quantifying relationships between abundances of cold-water coral Lophelia pertusa and terrain features: A case study on the Norwegian margin

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Cited by 19 publications
(10 citation statements)
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“…В частности, этот подход применялся для выявления и классификации ледников, покрытых плотной поверхностной мореной, которые на снимках сливаются с прилегающими долинами [Alifu et al, 2016[Alifu et al, , 2020, а также для выявления ледяных утесов водорослевых рифов [Marchese et al, 2020]. Использование моделей локальных величин и индексов шероховатости позволяет прогнозировать распределение колоний холодноводных кораллов [Tong et al, 2016;Bargain et al, 2017].…”
Section: Discussionunclassified
“…В частности, этот подход применялся для выявления и классификации ледников, покрытых плотной поверхностной мореной, которые на снимках сливаются с прилегающими долинами [Alifu et al, 2016[Alifu et al, , 2020, а также для выявления ледяных утесов водорослевых рифов [Marchese et al, 2020]. Использование моделей локальных величин и индексов шероховатости позволяет прогнозировать распределение колоний холодноводных кораллов [Tong et al, 2016;Bargain et al, 2017].…”
Section: Discussionunclassified
“…Noise present in the primary bathymetry and backscatter data layers can also be propagated, and even amplified in derivative layers [ 75 ], which can also affect model performance [ 50 ]. A decrease in spatial resolution can reduce data noise in derivative layers [ 46 , 67 ]. By averaging derivative data layers over an increasing area, noise can be smoothed out and made less distinct (see [ 32 ] for a comprehensive analysis of the effects of data coarsening on bathymetric derivatives).…”
Section: Discussionmentioning
confidence: 99%
“…Bottom currents transport sediments and control rates of erosion and deposition, making them one of the strongest drivers of sediment distribution [ 32 , 46 , 76 ]. Morphology influences the speed and orientation of currents, and also describes the exposure of seabed to them.…”
Section: Discussionmentioning
confidence: 99%
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“…At the more local scale, however, some terrain attributes, such as morphological features (topographic highs) and roughness, appear to be key contributors to CWC distribution (Dolan et al, 2008;Giusti et al, 2014;Rengstorf et al, 2014;Tong et al, 2016), where suitable environmental parameters for coral growth are present (in terms of temperature, salinity, dissolved oxygen, pH-values, and food availability). The interplay between local hydrodynamics and elevated features indeed promotes moderate to strong hydrodynamics and turbulent mixing, coupled with reduced terrigenous input and constant delivery of organic material, which in turn maintain CWC growth (White et al, 2005;Mienis et al, 2007).…”
Section: Introductionmentioning
confidence: 99%