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Record W4233907706 · doi:10.5194/amt-2020-184

Monitoring Sudden Stratospheric Warmings using radio occultation: a new approach demonstrated based on the 2009 event

2020· preprint· en· W4233907706 on OpenAlexaboutno aff
Ying Li, Gottfried Kirchengast, Marc Schwärz, Florian Ladstädter, Yunbin Yuan

Bibliographic record

Venuenot available
Typepreprint
Languageen
FieldEnvironmental Science
TopicClimate variability and models
Canadian institutionsnot available
FundersBundesministerium für Verkehr, Innovation und TechnologieÖsterreichische Forschungsförderungsgesellschaft
KeywordsLongitudeAltitude (triangle)Radio occultationSudden stratospheric warmingEnvironmental scienceAnomaly (physics)LatitudeMeteorologyEvent (particle physics)Atmospheric sciencesRemote sensingClimatologyPolar vortexGeodesyStratosphereGlobal Positioning SystemGeographyGeologyPhysicsComputer scienceMathematicsTelecommunicationsAstrophysics

Abstract

fetched live from OpenAlex

Abstract. We introduce a new method to detect and monitor Sudden Stratospheric Warming (SSW) events using Global Navigation Satellite System (GNSS) Radio Occultation (RO) data at high northern latitudes and demonstrate it for the well-known Jan–Feb 2009 event. We first construct RO temperature, density, and bending angle anomaly profiles and estimate vertical-mean anomalies in selected altitude layers. These mean anomalies are then averaged into a daily-updated 5° latitude × 20° longitude grid over 50° N–90° N. Based on the gridded mean anomalies, we employ the concept of Threshold Exceedance Areas (TEAs), the geographic areas wherein the anomalies exceed predefined threshold values such as 40 K or 40 %. We estimate five basic TEAs for selected altitude layers and thresholds and use them to derive primary-, secondary-, and trailing-phase TEA metrics to detect SSWs and to monitor in particular their main-phase (primary- plus secondary-phase) evolution on a daily basis. As an initial setting, the main-phase requires daily TEAs to exceed 3 Mio. km2, based on which main-phase duration, area, and overall event strength are recorded. Using the Jan–Feb 2009 SSW event for demonstration, and employing RO data plus cross-evaluation data from analysis fields of the European Centre for Medium-range Weather Forecasts (ECMWF), we find the new approach of strong potential for detecting and monitoring SSW events. The TEA metrics show a strong SSW emerging on Jan 17, reaching a maximum on Jan 23, and the strong primary-phase temperature anomaly fading by Jan 27. On Jan 22–23 a MSTA-TEA40 value (TEA of middle stratosphere temperature anomaly > 40 K) of about 9 Mio. km2 was reached. The geographic tracking of the SSW showed that it was centered over East Greenland, covering Greenland entirely and extending from Western Norway to Eastern Canada. The secondary- and trailing-phase metrics track the further SSW development, where the thermodynamic anomaly propagated downward and was fading with a transient upper stratospheric cooling, spanning until end February and beyond. Given the encouraging demonstration results, we expect the method very suitable for long-term monitoring of how SSW characteristics evolve under climate change and variability using both RO and reanalysis data.

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)0.001
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Simulation or modeling · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.008
Threshold uncertainty score0.015

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.001
Science and technology studies0.0000.000
Scholarly communication0.0010.000
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 head0.082
GPT teacher head0.282
Teacher spread0.199 · 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 designSimulation or modeling
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

Citations1
Published2020
Admission routes1
Has abstractyes

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