2014
DOI: 10.1016/j.dsr.2014.05.008
|View full text |Cite
|
Sign up to set email alerts
|

Seasonal and annual variability of vertically migrating scattering layers in the northern Arabian Sea

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1

Citation Types

2
22
0

Year Published

2015
2015
2022
2022

Publication Types

Select...
7
1
1

Relationship

0
9

Authors

Journals

citations
Cited by 30 publications
(24 citation statements)
references
References 46 publications
2
22
0
Order By: Relevance
“…In support of alternative explanations, Wang et al (2014) found that in the Persian Gulf light is a 407 dominant influence on scattering layer features and that temperature and salinity are as much or of more 408 importance than oxygen. In our dataset, Figure 9 shows several associations of scattering layers with 409 bends in plots of temperature vs. salinity, implying that at least some features (in addition to the shallow 410 features associated with the thermocline) are associated with boundaries between water masses.…”
Section: Association With Environmental Parameters 292mentioning
confidence: 96%
“…In support of alternative explanations, Wang et al (2014) found that in the Persian Gulf light is a 407 dominant influence on scattering layer features and that temperature and salinity are as much or of more 408 importance than oxygen. In our dataset, Figure 9 shows several associations of scattering layers with 409 bends in plots of temperature vs. salinity, implying that at least some features (in addition to the shallow 410 features associated with the thermocline) are associated with boundaries between water masses.…”
Section: Association With Environmental Parameters 292mentioning
confidence: 96%
“…Since then, various lines of evidence have converged on light being a first-order driver of DSL behaviour and therefore the most defining environmental factor for mesopelagic ecosystem structure (reviewed by Kaartvedt et al 2019). For example, DSL species change their depth distribution in response to the lunar cycle (Benoit-Bird et al 2009b, Wang et al 2014, Prihartato et al 2016) but also to short-term perturbations in light level from weather (Barham 1957, Kaartvedt et al 2017), eclipses (Backus et al 1965, Tont & Wick 1973, Kampa 1975, and variations in waters of changing transparency (Abookire et al 2002, Norheim et al 2016. Full moon, cloudless skies, and clear water cause deeper nocturnal scattering layers, with ramifications through the food chain because of reduced predation on zooplankton in the upper waters (Hernández-León et al 2010) and meso-pelagic fish being out of reach for many air-breathing predators (Horning & Trillmich 1999, Benoit-Bird et al 2009a.…”
Section: Introductionmentioning
confidence: 99%
“…The depth of the deep scattering layer varies depending on local conditions (Powell and Ohman ) and season (Wang et al. ). The distribution of food resources over the water column, and in particular the food availability in the deep scattering layer relative to the surface, will vary in reality and was simply postulated here.…”
Section: Discussionmentioning
confidence: 99%