Evidence map›Paper›PMID 31992702›Full record

ArticleNature communications2020

The Red Sea Deep Water is a potent source of atmospheric ethane and propane.

E Bourtsoukidis, A Pozzer, T Sattler, V N Matthaios, L Ernle, A Edtbauer, H Fischer, T Könemann, S Osipov, J-D Paris and 7 more

Open access · goldAbstract read
In one paragraph

Article in Nature communications, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 3 papers.

0numbers the graph read from it
0cells of the map it votes in
3citing papers in PubMed
4.8field-weighted citation impact, top 4% of its field
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

3 citing papers in PubMed, 60 citations in OpenAlex.

  1. Article
  2. Article
  3. Sources of indoor PMEnvironmental research · 2021
    Article
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

17 authors at 4 institutions in 4 countries.

E BourtsoukidisDepartment of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, 55128, Germany. e.bourtsoukidis@mpic.de.ORCID http://orcid.org/0000-0001-5578-9414
A PozzerDepartment of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, 55128, Germany.
T SattlerDepartment of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, 55128, Germany.
V N MatthaiosSchool of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, UK.
L ErnleDepartment of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, 55128, Germany.
A EdtbauerDepartment of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, 55128, Germany.
H FischerDepartment of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, 55128, Germany.
T KönemannDepartment of Multiphase Chemistry, Max Planck Institute for Chemistry, Mainz, 55128, Germany.
S OsipovDepartment of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, 55128, Germany.
J-D ParisLaboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS-UVSQ, UMR8212, IPSL, Gif-Sur-Yvette, France.
E Y PfannerstillDepartment of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, 55128, Germany.ORCID http://orcid.org/0000-0001-7715-1200
C StönnerDepartment of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, 55128, Germany.
I TadicDepartment of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, 55128, Germany.ORCID http://orcid.org/0000-0003-4419-2502
D WalterDepartment of Multiphase Chemistry, Max Planck Institute for Chemistry, Mainz, 55128, Germany.ORCID http://orcid.org/0000-0001-6807-5007
N WangDepartment of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, 55128, Germany.
J LelieveldDepartment of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, 55128, Germany.ORCID http://orcid.org/0000-0001-6307-3846
J WilliamsDepartment of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, 55128, Germany.
Max Planck Institute for Chemistry · DECyprus Institute · CYCentre National de la Recherche Scientifique · FRUniversity of Birmingham · GB

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Non-methane hydrocarbons (NMHCs) such as ethane and propane are significant atmospheric pollutants and precursors of tropospheric ozone, while the Middle East is a global emission hotspot due to  extensive oil and gas production. Here we compare in situ hydrocarbon measurements, performed around the Arabian Peninsula, with global model simulations that include current emission inventories (EDGAR) and state-of-the-art atmospheric circulation and chemistry mechanisms (EMAC model). While measurements of high mixing ratios over the Arabian Gulf are adequately simulated, strong underprediction by the model was found over the northern Red Sea. By examining the individual sources in the model and by utilizing air mass back-trajectory investigations and Positive Matrix Factorization (PMF) analysis, we deduce that Red Sea Deep Water (RSDW) is an unexpected, potent source of atmospheric NMHCs. This overlooked underwater source is comparable with total anthropogenic emissions from entire Middle Eastern countries, and significantly impacts the regional atmospheric chemistry.

Identifiers

PMID31992702
PMCPMC6987153
OpenAlexW3003402795

What OpenQuestion holds

Textmetadata
LicenceCC BY
Read underepoch 390

Registered trials

None linked

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.