Evidence map›Paper›PMID 41453962›Full record

ArticleScientific reports2025

Long-term hydrodynamic changes in marginal estuarine seas: the role of sea level rise and freshwater fluxes.

Emil V Stanev

Abstract read
In one paragraph

Article in Scientific reports, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

0numbers the graph read from it
0cells of the map it votes in
0citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

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.

2 · The registry

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.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

0 citing papers in PubMed.

No citing paper in PubMed yet.

4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

1 author.

Emil V StanevInstitute of Coastal Systems ‑ Analysis and Modeling, Helmholtz-Zentrum Hereon, Geesthacht, Germany. emil.stanev@hereon.de.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Significant environmental changes have occurred in marginal estuarine seas in the past, driven by changes in sea level and water and salt balances. Predicting the future evolution of these seas is a scientific challenge because adequate scenario studies are currently hindered by the quality of 3D models on millennial timescales. In this paper, we present relatively simple and efficient models of the Black Sea. This sea connects rivers to the ocean and acts as a 'mixer', diluting inflowing saline ocean water with riverine freshwater to generate brackish water. For such an ocean system, it is crucial to incorporate mixing within the sea and two-layer exchange within the strait into a single framework. This paper demonstrates that the developed models can be used to (1) estimate past and future ocean states resulting from specific combinations of global sea level and freshwater fluxes; (2) critically address the consistency of used water and salt balances; (3) conceptualizing further studies of major environmental trends. Illustrations are provided to show the evolution of stratification of the Black Sea in the Holocene. Application to other ocean environments controlled by two-layer exchange flows is also discussed.

Identifiers

PMID41453962
PMCPMC12749219

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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.