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  Global climatology of Convective Available Potential Energy (CAPE) and Convective Inhibition (CIN) in ERA-40 reanalysis

Riemann-Campe, K., Fraedrich, K., & Lunkeit, F. (2009). Global climatology of Convective Available Potential Energy (CAPE) and Convective Inhibition (CIN) in ERA-40 reanalysis. Atmospheric Research, 93(1-3), 534-545. doi:10.1016/j.atmosres.2008.09.037.

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 Creators:
Riemann-Campe, Kathrin1, Author
Fraedrich, Klaus2, Author
Lunkeit, Frank3, 4, Author           
Affiliations:
1IMPRS on Earth System Modelling, MPI for Meteorology, Max Planck Society, Bundesstraße 53, 20146 Hamburg, DE, ou_913547              
2external, ou_persistent22              
3A 2 - Climate Processes and Feedbacks, Research Area A: Climate Dynamics and Variability, The CliSAP Cluster of Excellence, External Organizations, ou_1863497              
4A 1 - Climate Variability and Predictability, Research Area A: Climate Dynamics and Variability, The CliSAP Cluster of Excellence, External Organizations, ou_1863478              

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Free keywords: SEVERE THUNDERSTORM; PARAMETERS; SUPERCELLSCAPE; CIN; ERA-40; Trend analysis;
 Abstract: Convective Available Potential Energy (CAPE) and Convective Inhibition (CIN) play a dominant role in convective precipitation, its genesis and intensity. A global climatology of CAPE and CIN is presented in terms of seasonal means, variances, and trends based on 44 years (1958-2001) of six-hourly ERA-40 reanalysis (European Centre for Medium-Range Weather Forecast ECMWF, T106 resolution). CAPE shows large values and high variability in the tropics with maxima over the continents; the seasonal changes are dominated by specific humidity. CIN shows large means and variability in the subtropics. Significant trends in CAPE and CIN give the following results: (i) In general, a CAPE increase is noted during all seasons while, in particular, in autumn CIN shows a decrease over continents. (ii) Splitting of the time series reveals a sign change in trend commencing at the end of the 70s; this is observed in parts of the tropical continents and North America. CAPE and CIN show trends of opposite sign with CAPE increasing in the first half and a decrease during the second half (and vice versa for CIN). (c) 2008 Elsevier B.V. All rights reserved.

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Language(s): eng - English
 Dates: 2009-07
 Publication Status: Issued
 Pages: -
 Publishing info: -
 Table of Contents: -
 Rev. Type: Peer
 Degree: -

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Title: Atmospheric Research
Source Genre: Journal
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Publ. Info: Amsterdam, Netherlands : Elsevier
Pages: - Volume / Issue: 93 (1-3) Sequence Number: - Start / End Page: 534 - 545 Identifier: ISSN: 0169-8095
CoNE: https://pure.mpg.de/cone/journals/resource/958480211574