ReviewPhilosophical transactions. Series A, Mathematical, physical, and engineering sciences2022
Wave propagation in the marginal ice zone: connections and feedback mechanisms within the air-ice-ocean system.
Review in Philosophical transactions. Series A, Mathematical, physical, and engineering sciences, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.
What it found
Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.
The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
The trial behind it
Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.
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Who cites it
5 citing papers in PubMed, 49 citations in OpenAlex.
- Revealing the Antarctic marginal ice zone with a decade-long wave-in-ice climatology.Nature communications · 2026Article
- Floes, the marginal ice zone and coupled wave-sea-ice feedbacks.Philosophical transactions. Series A, Mathematical, physical, and engineering sciences · 2022Review
- Theory, modelling and observations of marginal ice zone dynamics: multidisciplinary perspectives and outlooks.Philosophical transactions. Series A, Mathematical, physical, and engineering sciences · 2022Article
- Modelling attenuation of irregular wave fields by artificial ice floes in the laboratory.Philosophical transactions. Series A, Mathematical, physical, and engineering sciences · 2022Article
- Marginal ice zone dynamics: future research perspectives and pathways.Philosophical transactions. Series A, Mathematical, physical, and engineering sciences · 2022Review
Corrections and comments
PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.
Authors and funding
1 author at 1 institution in 1 country.
Funding
No grant is acknowledged in the PubMed record.
Abstract
The propagation of ocean surface waves within the marginal ice zone (MIZ) is a defining phenomenon of this dynamic zone. Over decades of study, a variety of methods have been developed to observe and model wave propagation in the MIZ, with a common focus of determining the attenuation of waves with increasing distance into the MIZ. More recently, studies have begun to explore the consequences of wave attenuation and the coupled processes in the air-ice-ocean-land system. Understanding these coupled processes and effects is essential for accurate high-latitude forecasts. As waves attenuate, their momentum and energy are transferred to the sea ice and upper ocean. This may compact or expand the MIZ, depending on the conditions, while simultaneously modulating the wind work on the system. Wave attenuation is also a key process in coastal dynamics, where land-fast ice has historically protected both natural coasts and coastal infrastructure. With observed trends of increasing wave activity and retreating seasonal ice coverage, the propagation of waves within the MIZ is increasingly important to regional and global climate trends. This article is part of the theme issue 'Theory, modelling and observations of marginal ice zone dynamics: multidisciplinary perspectives and outlooks'.
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Registered trials
Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.