Температурные контрасты осенних месяцев 2014 года в России
Notice bibliographique
Résumé
The main cause of the weather (and climate) anomalies is the fluctuations of total ozone in the atmosphere. These fluctuations are caused by (i) emission of the deep ozone-depleting gases (hydrogen and methane), and (ii) variations of the geomagnetic field, which increase the concentration of ozone. The positive ozone anomalies cool the troposphere and create anti-cyclones, dry, heavy and slow moving air masses. The negative anomalies warm up the air and create the cyclonic masses with law pressure. The closest anticyclones could move to that area bringing with them the anomalous temperatures, sometimes very high and sometimes very law. In my subheading, I analyze temperature anomalies of autumn 2014 in These anomalies were about ten-day duration and alternated. So, starting in September, the anomalous heat rhythmically was replaced by abnormal cold, which in the end of November reached values typical for January. The causes of the temperature anomalies were synchronous total ozone anomalies. Stable ozone hole in the northern part of European Russia played the main role in this process. Southern anticyclones, which bringing the anomalous heat, was periodically drawn into this hole. In November, the anticyclone, which was formed in Siberia and which was brought the ‘January’ frosts in European Russia, even in its southern provinces, was also drawn into in this hole. weather (climate) anomaly; anomalies of ozone; ozone layer; deep degassing; hydrogen; snowfalls; frosts About Successes of the Russian Winter. GISMETEO News. N.p., 6 Nov. 2014. Web. . (In Russian). Due to Ыnowfall, There Were 641 Accidents per 48 Hours in the Perm Region. GISMETEO News. N.p., 20 Oct. 2014. Web. . (In Russian). Golubov B.N. Reflection on the Amazing Information the Geological, Environmental and Political Aspects of the Storage and Disposal of Nuclear Materials. Space and Time 2 (2012): 224–228. (In Russian). Hot September: Anomalies in Siberia, in Russia and in the World. Ermak-info. N.p., 1 Oct. 2014. Web. . (In Russian). Hydrometeorological Centre of Major Weather and Climatic Features in September 2014 in the Northern Hemisphere. Hydrometeorological Centre of Russia: About Weather – At First Hand. Federal Service for Hydrometeorology and Environmental Monitoring, n.d. Web. . (In Russian). Hydrometeorological Centre of Major Weather and Climatic Features of October 2014 in the Northern Hemisphere. Hydrometeorological Centre of Russia: About Weather – At First Hand. Federal Service for Hydrometeorology and Environmental Monitoring, n.d. Web. . (In Russian). In January, Frosts Came to Chernozemye. GISMETEO News. N.p., 26 Nov. 2014. Web . (In Russian). In Russia, the Abnormal Frosts Are Amplified. GISMETEO News. N.p., 25 Nov. 2014. Web. . Major Weather and Climatic Features in November 2014 in the Northern Hemisphere. Hydrometeorological Centre of Russia: About Weather – At First Hand. Federal Service for Hydrometeorology and Environmental Monitoring, n.d. Web. . (In Russian). November Ended with Anomalous Frosts. GISMETEO News. N.p., 30 Nov. 2014. Web. . (In Russian). Premature Snowfalls in the Perm Region Destroyed Harvest of Cabbage. GISMETEO News. N.p., 24 Nov. 2014. Web. . (In Russian). Select Ozone Maps. Ozone and Ultraviolet Research and Monitoring. Environment Canada's World Wide Web Site. The Green LaneTM. Web. . Syvorotkin V.L. Uselessness of the Montreal Protocol To Save the Earth's Ozone Layer. Space and Time 3 (2014): 256–265. (In Russian). There Is a Record Atmospheric Pressure in Moscow!. Phobos. N.p., 10 June 2014. Web. . (In Russian). There is Minus 50° C in Siberia!. GISMETEO News. 24.11 2014. Web. . (In Russian). Two Anomalies in November in Chernozemye. GISMETEO News. N.p., 1 Dec. 2014. Web . (In Russian). Weather in Russia Has Mixed Climate Zones. GISMETEO News. N.p., 27 Nov. 2014. Web. . (In Russian). Syvorotkin, V. L. Temperature Contrasts in the Autumn Months of 2014 in Russia. Space and Time 4 (2014): 222–229. (In Russian). Fixed network address 2226-7271provr_st4-18.2014.102.
Récupéré en direct depuis OpenAlex et désinversé. Les résumés ne sont pas conservés dans cette base de données : les index inversés représentent 8,6 Go des 9,3 Go de texte de la base, et le serveur dispose de 13 Go libres.
Comment cette classification a été obtenuedéplier
Prédiction distillée sur la base complète
Imitation des enseignantsNi prévalence calibrée, ni vérité terrain. Validation humaine à venir. Apprise à partir de 10 348 étiquettes directes de Codex et de 10 348 étiquettes directes de Gemma. Le mode candidate est l'union des têtes enseignantes seuillées; le consensus est leur intersection. Ces sorties portent le statut machine_predicted_unvalidated et ne sont ni des étiquettes humaines ni des étiquettes directes de modèles de pointe.
Scores Codex et Gemma par catégorie
| Catégorie | Codex | Gemma |
|---|---|---|
| Métarecherche | 0,001 | 0,000 |
| Méta-épidémiologie (sens strict) | 0,001 | 0,001 |
| Méta-épidémiologie (sens large) | 0,001 | 0,001 |
| Bibliométrie | 0,000 | 0,001 |
| Études des sciences et des technologies | 0,001 | 0,002 |
| Communication savante | 0,000 | 0,001 |
| Science ouverte | 0,002 | 0,001 |
| Intégrité de la recherche | 0,001 | 0,001 |
| Charge utile insuffisante (le modèle a refusé de juger) | 0,024 | 0,037 |
Scores machine (provisoires)
Les deux têtes enseignantes du modèle étudiant, lues sur ce travail. Un score ordonne la base pour la relecture; il n'affirme jamais une catégorie, et le statut de validation accompagne chaque rangée tel quel.
Scores de référence d'un modèle non mature (critères de maturité non atteints, 7 itérations). Un score ordonne; il n'affirme jamais une catégorie.
score_only:v0-immature-baseline · tel quel depuis la passe de notation : score_only signifie que le nombre peut ordonner les travaux, et qu'aucune étiquette de catégorie n'en découleClassification
machine, non validéePrédiction automatique; les deux têtes enseignantes s’accordent sur ce qui est montré ici.
Le détail, modèle par modèle et score par score, se trouve en fin de page sous « Comment cette classification a été obtenue ».