MétaCan
Menu
← Back to cohort
Record W4408475218 · doi:10.5194/egusphere-egu25-9344

Enhanced inorganic iodine in the upper troposphere potentially driven by elevated emission and/or fast vertical transport by tropical cyclone

2025· preprint· en· W4408475218 on OpenAlexaff
Karolin Voss, Benjamin Weyland, A. Butz, Valentin Lauther, C.Michael Volk, Bärbel Vogel, Andreas Engel, Tanja Schuck, Timo Keber, Meike Rotermund, Klaus Pfeilsticker

Bibliographic record

Venuenot available
Typepreprint
Languageen
FieldEarth and Planetary Sciences
TopicAtmospheric Ozone and Climate
Canadian institutionsUniversity of Toronto
Fundersnot available
KeywordsTroposphereTropical cycloneEnvironmental scienceClimatologyAtmospheric sciencesCyclone (programming language)MeteorologyGeologyGeography

Abstract

fetched live from OpenAlex

Halogens are known to deplete ozone both in the troposphere and stratosphere. As the source distribution and thus the local contribution of chlorine and bromine containing species to atmospheric ozone depletion is reasonably well known, the respective role of iodine containing species is subject of current research. In contrast to the major sources of chlorine in the stratosphere which derive from man-made chlorinated hydrocarbons, about half of stratospheric bromine stems from bromocarbons of natural origin while iodine predominantly originates from inorganic species (I2, and HOI) emitted from the oceans. It has been indicated previously that tropical cyclones emit elevated amounts of brominated species (e.g. CHBr3 and CH2Br2) which are efficiently transported into the extratropical upper troposphere and eventually into the lower stratosphere. Here we provide evidence that also significant amounts of inorganic iodine emitted from the ocean surface and/or through sea-spray are transported to the extratropical upper troposphere through tropical cyclone driven fast vertical transport.Our finding is based on the simultaneous detection of elevated amounts of brominated very short-lived substances (VSLS) and iodine oxide (IO, ~0.3 pptv) while simultaneously relatively low mixing ratios of the anthropogenically emitted CH2Cl2 were measured in the upper troposphere (~13 km, θ~360 K) of the mid-Atlantic on October 1st,2017. CLaMS back-trajectory calculations driven by ECMWF ERA-Interim reanalysis suggest that these iodine-rich air masses originate from marine surface air masses being uplifted by the category 5 hurricane Maria.The measurements were performed from aboard HALO (High Altitude and LOng range Aircraft) during the WISE (Wave-driven ISentropic Exchange) campaign over the mid-Atlantic in September and October 2017. IO was detected in limb scattered skylight using the miniDOAS instrument, while the organic chlorinated and brominated species were detected by the HAGAR-V and GhOST GC/MS instruments.Our findings suggest that tropical storms lead to elevated emissions of inorganic iodine rapidly transported from the tropical marine boundary layer into the upper troposphere. This mechanism implies a potentially significant role of iodine in ozone destruction in the remnant air of tropical storms and a possible pathway for iodine to enter the lower stratosphere in significant amounts.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.012
Threshold uncertainty score0.023

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.006
GPT teacher head0.215
Teacher spread0.208 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations0
Published2025
Admission routes1
Has abstractyes

Explore more

Same topicAtmospheric Ozone and Climate→French-language works237,207→