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Amplified mid-latitude planetary waves favour particular regional weather extremes

Author
SCREEN, James A1 ; SIMMONDS, Ian2
[1] College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter EX4 4QF, United Kingdom
[2] School of Earth Sciences, The University of Melbourne, Melbourne, Victoria 3010, Australia
Source

Nature climate change (Print). 2014, Vol 4, Num 8, pp 704-709, 6 p ; ref : 30 ref

ISSN
1758-678X
Scientific domain
Global change; Ecology; Hydrology, water resources; Climatology, meteorology
Publisher
Nature Publishing Group, London
Publication country
United Kingdom
Document type
Article
Language
English
Keyword (fr)
Analyse série temporelle Donnée observation Fréquence apparition Hémisphère Nord Moyenne latitude Onde atmosphérique Onde planétaire Onde stationnaire Phase amplitude Troposphère Evénement extrême
Keyword (en)
time series analysis Observation data Occurrence frequency Northern Hemisphere Mid latitude Atmospheric wave Planetary wave Standing wave Amplitude phase troposphere Extreme event
Keyword (es)
Dato observación Frecuencia aparición Hemisferio norte Latitud media Onda atmosférica Onda planetaria Onda estacionaria Fase amplitud Acontecimiento extremo
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E02 External geophysics / 001E02D Meteorology / 001E02D01 General circulation. Atmospheric waves

Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E02 External geophysics / 001E02D Meteorology / 001E02D10 Climatology. Bioclimatology. Climate change

Discipline
External geophysics
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
28641939

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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