Super‐Clausius–Clapeyron scaling of rainfall in a model squall line

The sensitivity of squall rainfall to changes in atmospheric temperature is investigated. For instantaneous rainrates and accumulations up to one hour, extreme rainfall scales with Clausius‐Clapeyron (CC) for temperatures below 24°C and at up to twice CC above 24°C. For longer accumulation periods a...

Full description

Saved in:
Bibliographic Details
Published in:Quarterly journal of the Royal Meteorological Society Vol. 139; no. 671; pp. 334 - 339
Main Authors: Singleton, Andrew, Toumi, Ralf
Format: Journal Article
Language:English
Published: Chichester, UK John Wiley & Sons, Ltd 01.01.2013
Wiley Subscription Services, Inc
Subjects:
Accumulations
Atmospheric temperature
Clausius–Clapeyron scaling
Climate change
Copyrights
Design parameters
Extreme weather
Flooding
High temperature
PMP
probable maximum precipitation
Rainfall
rainfall extremes
Reproduction
Squalls
ISSN:0035-9009, 1477-870X
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Abstract The sensitivity of squall rainfall to changes in atmospheric temperature is investigated. For instantaneous rainrates and accumulations up to one hour, extreme rainfall scales with Clausius‐Clapeyron (CC) for temperatures below 24°C and at up to twice CC above 24°C. For longer accumulation periods and higher temperatures the scaling breaks down due to increased propagation of the squall line. For all periods, the storm average rainfall is found to scale at approximately 1.5 times CC over the entire range of temperatures. These results have implications for design parameters for infrastructure that is vulnerable to flooding and for climate change projections. Copyright © 2012 Royal Meteorological Society
AbstractList The sensitivity of squall rainfall to changes in atmospheric temperature is investigated. For instantaneous rainrates and accumulations up to one hour, extreme rainfall scales with Clausius‐Clapeyron (CC) for temperatures below 24°C and at up to twice CC above 24°C. For longer accumulation periods and higher temperatures the scaling breaks down due to increased propagation of the squall line. For all periods, the storm average rainfall is found to scale at approximately 1.5 times CC over the entire range of temperatures. These results have implications for design parameters for infrastructure that is vulnerable to flooding and for climate change projections. Copyright © 2012 Royal Meteorological Society
The sensitivity of squall rainfall to changes in atmospheric temperature is investigated. For instantaneous rainrates and accumulations up to one hour, extreme rainfall scales with Clausius-Clapeyron (CC) for temperatures below 24 degree C and at up to twice CC above 24 degree C. For longer accumulation periods and higher temperatures the scaling breaks down due to increased propagation of the squall line. For all periods, the storm average rainfall is found to scale at approximately 1.5 times CC over the entire range of temperatures. These results have implications for design parameters for infrastructure that is vulnerable to flooding and for climate change projections. Copyright [copy 2012 Royal Meteorological Society
The sensitivity of squall rainfall to changes in atmospheric temperature is investigated. For instantaneous rainrates and accumulations up to one hour, extreme rainfall scales with Clausius-Clapeyron (CC) for temperatures below 24°C and at up to twice CC above 24°C. For longer accumulation periods and higher temperatures the scaling breaks down due to increased propagation of the squall line. For all periods, the storm average rainfall is found to scale at approximately 1.5 times CC over the entire range of temperatures. These results have implications for design parameters for infrastructure that is vulnerable to flooding and for climate change projections. Copyright © 2012 Royal Meteorological Society [PUBLICATION ABSTRACT]
Author Toumi, Ralf
Singleton, Andrew
Author_xml – sequence: 1
  givenname: Andrew
  surname: Singleton
  fullname: Singleton, Andrew
– sequence: 2
  givenname: Ralf
  surname: Toumi
  fullname: Toumi, Ralf
  email: r.toumi@imperial.ac.uk
BookMark eNqF0MFKAzEQBuAgFWyr-AoLHhRk6ySbzWaPUrQqBREVvIU0m5WUNGmTLtJbH0HwDfskbq0nUYSBGZKPgfl7qOO80wgdYxhgAHKxmA5wics91MW0KFJewEsHdQGyPC0BygPUi3EKAHlBii4aPTZzHTbr96GVTTRN3Kw_2nGuV8G7JCppjXtNfJ0EaVwtrU2MS2Qy85W2SVw025eW6EO03_5GffTd--j5-uppeJOO70e3w8txqijBZaqqTLNcASGccTbJK6zwBPiEVTTXdUFwVnJeTdrCJGMVAawqLUmlMsUlU3XWR2e7vfPgF42OSzEzUWlrpdO-iQIzSgjlrID_Kc0oYJ7TLT35Qae-Ca49ROAMF4wAy2mrTndKBR9j0LWYBzOTYSUwiG32YjEV2-xbmf6Qyizl0ni3bHO0v_jznX8zVq_-Wise7r70J5aBlds
CitedBy_id crossref_primary_10_1007_s40641_020_00157_9
crossref_primary_10_1038_s41598_020_67088_1
crossref_primary_10_5194_hess_22_3777_2018
crossref_primary_10_1029_2018JD029954
crossref_primary_10_1038_ngeo2456
crossref_primary_10_1002_2014RG000464
crossref_primary_10_1002_2015JD024286
crossref_primary_10_1007_s00382_020_05462_5
crossref_primary_10_1029_2012GL052945
crossref_primary_10_1038_nature22069
crossref_primary_10_5194_acp_19_1471_2019
crossref_primary_10_1175_JHM_D_17_0158_1
crossref_primary_10_1088_1748_9326_adf07d
crossref_primary_10_1007_s00704_019_03062_w
crossref_primary_10_1016_j_wace_2021_100391
crossref_primary_10_1029_2023JD039473
crossref_primary_10_1016_j_jhydrol_2016_12_002
crossref_primary_10_1002_joc_5799
crossref_primary_10_1007_s10584_019_02523_5
crossref_primary_10_1038_ngeo2789
crossref_primary_10_1038_ngeo1731
crossref_primary_10_1175_JCLI_D_21_0436_1
crossref_primary_10_1029_2019JD031026
crossref_primary_10_1175_JCLI_D_18_0050_1
crossref_primary_10_1007_s00382_018_4153_z
crossref_primary_10_1038_s43017_020_00128_6
crossref_primary_10_1002_2016GL071285
crossref_primary_10_1007_s12040_023_02064_7
crossref_primary_10_1029_2020WR028387
crossref_primary_10_1007_s00382_016_3083_x
crossref_primary_10_1038_s41598_018_38071_8
crossref_primary_10_1007_s40641_021_00177_z
crossref_primary_10_3390_atmos11080786
crossref_primary_10_1002_joc_4678
crossref_primary_10_1029_2017GL076874
crossref_primary_10_1002_2013JD020868
crossref_primary_10_1038_s41598_024_71662_2
crossref_primary_10_1088_1748_9326_ab7130
crossref_primary_10_5194_acp_20_6207_2020
crossref_primary_10_1029_2019GL086927
crossref_primary_10_1029_2020GL091371
crossref_primary_10_1002_2015JD023497
crossref_primary_10_1007_s11430_022_9953_0
crossref_primary_10_1007_s40641_015_0009_3
crossref_primary_10_1029_2022EF002833
crossref_primary_10_1175_JCLI_D_12_00655_1
crossref_primary_10_1002_2017JD027012
crossref_primary_10_1175_JCLI_D_20_0194_1
crossref_primary_10_3389_feart_2023_1093543
crossref_primary_10_1088_1748_9326_ab5638
crossref_primary_10_1016_j_atmosres_2024_107265
crossref_primary_10_1088_1748_9326_ade607
crossref_primary_10_1029_2018GL077716
crossref_primary_10_1029_2021MS002607
crossref_primary_10_1038_s41612_020_0117_1
crossref_primary_10_1088_1748_9326_9_1_014003
crossref_primary_10_3390_e19120685
crossref_primary_10_1175_JCLI_D_16_0808_1
crossref_primary_10_1175_JCLI_D_17_0075_1
crossref_primary_10_1088_1748_9326_10_8_085001
crossref_primary_10_1016_j_quascirev_2017_06_002
crossref_primary_10_1029_2018GL080516
crossref_primary_10_1038_s41561_025_01686_4
crossref_primary_10_1002_2016JD025285
crossref_primary_10_1029_2022GL100624
crossref_primary_10_1080_16000870_2017_1373578
crossref_primary_10_1088_1748_9326_add753
crossref_primary_10_1016_j_jhydrol_2020_125249
crossref_primary_10_1016_j_jhydrol_2016_04_070
Cites_doi 10.1029/2009JD012008
10.1038/ngeo262
10.1029/2009GL040218
10.1029/2005GL022465
10.1175/JCLI3990.1
10.1088/1748-9326/5/2/025208
10.1038/nature01092
10.1007/s00382-006-0180-2
10.1175/1520-0469(1988)045<1990:SAEONS>2.0.CO;2
10.1029/2004RG000150
10.1175/BAMS-84-9-1205
10.1016/0022-1694(95)02953-2
10.1029/1998WR900013
10.1175/2009JCLI2701.1
10.1038/ngeo523
ContentType Journal Article
Copyright Copyright © 2012 Royal Meteorological Society
Copyright_xml – notice: Copyright © 2012 Royal Meteorological Society
DBID 24P
AAYXX
CITATION
7TG
7TN
F1W
H96
KL.
L.G
8FD
H8D
L7M
DOI 10.1002/qj.1919
DatabaseName Wiley Online Library Open Access
CrossRef
Meteorological & Geoastrophysical Abstracts
Oceanic Abstracts
ASFA: Aquatic Sciences and Fisheries Abstracts
Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources
Meteorological & Geoastrophysical Abstracts - Academic
Aquatic Science & Fisheries Abstracts (ASFA) Professional
Technology Research Database
Aerospace Database
Advanced Technologies Database with Aerospace
DatabaseTitle CrossRef
Aquatic Science & Fisheries Abstracts (ASFA) Professional
Meteorological & Geoastrophysical Abstracts
Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources
Oceanic Abstracts
Meteorological & Geoastrophysical Abstracts - Academic
ASFA: Aquatic Sciences and Fisheries Abstracts
Technology Research Database
Aerospace Database
Advanced Technologies Database with Aerospace
DatabaseTitleList CrossRef

Technology Research Database
Aquatic Science & Fisheries Abstracts (ASFA) Professional
Aquatic Science & Fisheries Abstracts (ASFA) Professional
Database_xml – sequence: 1
  dbid: 24P
  name: Wiley Online Library Open Access
  url: https://authorservices.wiley.com/open-science/open-access/browse-journals.html
  sourceTypes: Publisher
DeliveryMethod fulltext_linktorsrc
Discipline Meteorology & Climatology
EISSN 1477-870X
EndPage 339
ExternalDocumentID 2920817351
10_1002_qj_1919
QJ1919
Genre article
GrantInformation_xml – fundername: Flood Risk from Extreme Events
  funderid: NE/F011822/1
– fundername: Natural Environment Research Council
GroupedDBID -~X
.3N
.GA
.Y3
05W
0R~
10A
123
1L6
1OB
1OC
1ZS
24P
31~
33P
3SF
3WU
4.4
50Y
50Z
51W
51X
52M
52N
52O
52P
52S
52T
52U
52W
52X
5VS
66C
6TJ
702
7PT
8-0
8-1
8-3
8-4
8-5
8UM
930
A03
AAESR
AAEVG
AAHQN
AAMMB
AAMNL
AANHP
AANLZ
AAONW
AASGY
AAXRX
AAYCA
AAZKR
ABCQN
ABCUV
ABEFU
ABEML
ABJNI
ACAHQ
ACBWZ
ACCZN
ACGFS
ACPOU
ACPRK
ACRPL
ACSCC
ACXBN
ACXQS
ACYXJ
ADBBV
ADEOM
ADIZJ
ADKYN
ADMGS
ADMLS
ADNMO
ADOZA
ADXAS
ADZMN
AEFGJ
AEIGN
AEIMD
AENEX
AEUYR
AEYWJ
AFBPY
AFFNX
AFFPM
AFGKR
AFWVQ
AGHNM
AGQPQ
AGXDD
AGYGG
AHBTC
AIDQK
AIDYY
AIQQE
AITYG
AIURR
AJXKR
ALAGY
ALMA_UNASSIGNED_HOLDINGS
ALUQN
ALVPJ
AMBMR
AMYDB
ASPBG
ATUGU
AUFTA
AVWKF
AZBYB
AZFZN
AZVAB
BAFTC
BDRZF
BFHJK
BHBCM
BMNLL
BNHUX
BROTX
BRXPI
BY8
CS3
D-E
D-F
DCZOG
DDYGU
DPXWK
DR2
DRFUL
DRSTM
DU5
EBS
EJD
F00
F01
F04
FEDTE
G-S
G.N
GODZA
H.T
H.X
HBH
HF~
HGLYW
HVGLF
HZ~
H~9
IX1
J0M
JPC
LATKE
LAW
LC2
LC3
LEEKS
LH4
LITHE
LOXES
LP6
LP7
LUTES
LW6
LYRES
M62
MEWTI
MK4
MRFUL
MRSTM
MSFUL
MSSTM
MXFUL
MXSTM
N04
N05
NF~
NNB
O66
O9-
OHT
OK1
P2P
P2W
P2X
P4D
PALCI
Q.N
Q11
QB0
QRW
R.K
RIWAO
RJQFR
ROL
RX1
SAMSI
SUPJJ
UB1
VOH
W8V
W99
WBKPD
WIB
WIH
WIK
WJL
WOHZO
WQJ
WUPDE
WXSBR
WYISQ
XG1
XV2
ZY4
ZZTAW
~02
~IA
~WT
AAYXX
ABUFD
CITATION
O8X
7TG
7TN
F1W
H96
KL.
L.G
8FD
H8D
L7M
ID FETCH-LOGICAL-c4219-cd3e65c0228686b5d1c1b08b6d45ef7213988db8db1236d201cdea2dc3c8a6cf3
IEDL.DBID 24P
ISICitedReferencesCount 81
ISICitedReferencesURI http://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=Summon&SrcAuth=ProQuest&DestLinkType=CitingArticles&DestApp=WOS_CPL&KeyUT=000316623700006&url=https%3A%2F%2Fcvtisr.summon.serialssolutions.com%2F%23%21%2Fsearch%3Fho%3Df%26include.ft.matches%3Dt%26l%3Dnull%26q%3D
ISSN 0035-9009
IngestDate Fri Jul 11 09:17:50 EDT 2025
Thu Jul 10 23:11:31 EDT 2025
Sun Jul 06 02:41:33 EDT 2025
Tue Nov 18 21:33:48 EST 2025
Sat Nov 29 01:49:49 EST 2025
Sun Sep 21 06:19:36 EDT 2025
IsDoiOpenAccess true
IsOpenAccess true
IsPeerReviewed true
IsScholarly true
Issue 671
Language English
LinkModel DirectLink
MergedId FETCHMERGED-LOGICAL-c4219-cd3e65c0228686b5d1c1b08b6d45ef7213988db8db1236d201cdea2dc3c8a6cf3
Notes ObjectType-Article-1
SourceType-Scholarly Journals-1
content type line 14
ObjectType-Feature-2
content type line 23
OpenAccessLink https://onlinelibrary.wiley.com/doi/abs/10.1002%2Fqj.1919
PQID 1317620654
PQPubID 1016432
PageCount 6
ParticipantIDs proquest_miscellaneous_1642248670
proquest_miscellaneous_1434018540
proquest_journals_1317620654
crossref_primary_10_1002_qj_1919
crossref_citationtrail_10_1002_qj_1919
wiley_primary_10_1002_qj_1919_QJ1919
PublicationCentury 2000
PublicationDate January 2013 Part B
PublicationDateYYYYMMDD 2013-01-01
PublicationDate_xml – month: 01
  year: 2013
  text: January 2013 Part B
PublicationDecade 2010
PublicationPlace Chichester, UK
PublicationPlace_xml – name: Chichester, UK
– name: Reading
PublicationTitle Quarterly journal of the Royal Meteorological Society
PublicationYear 2013
Publisher John Wiley & Sons, Ltd
Wiley Subscription Services, Inc
Publisher_xml – name: John Wiley & Sons, Ltd
– name: Wiley Subscription Services, Inc
References 2007; 28
2009; 22
2009; 36
2004; 42
2006; 42
1999; 35
1996; 183
2008
1988; 45
2006; 19
2005; 32
2002; 419
2008; 1
2009; 2
2010; 5
2003; 84
2009; 114
e_1_2_6_10_1
Hong S‐Y (e_1_2_6_8_1) 2006; 42
e_1_2_6_9_1
e_1_2_6_5_1
e_1_2_6_4_1
e_1_2_6_7_1
e_1_2_6_6_1
e_1_2_6_13_1
e_1_2_6_14_1
e_1_2_6_3_1
e_1_2_6_11_1
e_1_2_6_2_1
e_1_2_6_12_1
e_1_2_6_17_1
e_1_2_6_18_1
e_1_2_6_15_1
e_1_2_6_16_1
References_xml – volume: 36
  start-page: L17702
  year: 2009
  article-title: Temperature dependence of global precipitation extremes
  publication-title: Geophys. Res. Lett.
– volume: 2
  start-page: 372
  year: 2009
  end-page: 373
  article-title: Unexpected rise in extreme precipitation caused by a shift in rain type?
  publication-title: Nature Geosci
– volume: 114
  start-page: D18102
  year: 2009
  article-title: Seasonal characteristics of the relationship between daily precipitation intensity and surface temperature
  publication-title: J. Geophys. Res.
– volume: 42
  start-page: RG4003
  year: 2004
  article-title: Mesoscale convective systems
  publication-title: Rev. Geophys.
– year: 2008
– volume: 22
  start-page: 5676
  year: 2009
  end-page: 5685
  article-title: Scaling of precipitation extremes over a wide range of climates studied with an idealized GCM
  publication-title: J. Climate
– volume: 419
  start-page: 224
  year: 2002
  end-page: 232
  article-title: Constraints on future changes in climate and the hydrologic cycle
  publication-title: Nature
– volume: 5
  start-page: 025208
  year: 2010
  article-title: Linking increases in hourly precipitation extremes to atmospheric temperature and moisture changes
  publication-title: Environ. Res. Lett.
– volume: 45
  start-page: 1990
  year: 1988
  end-page: 2013
  article-title: Structure and evolution of numerically simulated squall lines
  publication-title: J. Atmos. Sci.
– volume: 32
  start-page: L14812
  year: 2005
  article-title: A fundamental probability distribution for heavy rainfall
  publication-title: Geophys. Res. Lett.
– volume: 1
  start-page: 511
  year: 2008
  end-page: 514
  article-title: Increase in hourly precipitation extremes beyond expectations from temperature changes
  publication-title: Nature Geosci.
– volume: 35
  start-page: 785
  year: 1999
  end-page: 796
  article-title: A numerical modeling study to investigate the assumptions used in the calculation of probable maximum precipitation
  publication-title: Water Resour. Res.
– volume: 28
  start-page: 351
  year: 2007
  end-page: 363
  article-title: Testing the Clausius–Clapeyron constraint on changes in extreme precipitation under CO warming
  publication-title: Clim. Dyn.
– volume: 84
  start-page: 1205
  year: 2003
  end-page: 1217
  article-title: The changing character of precipitation
  publication-title: Bull. Am. Meteorol. Soc.
– volume: 183
  start-page: 277
  year: 1996
  end-page: 306
  article-title: Estimating probable maximum precipitation using a storm model approach
  publication-title: J. Hydrol.
– volume: 42
  start-page: 129
  year: 2006
  end-page: 151
  article-title: The WRF single‐moment 6‐class microphysics scheme (WSM6)
  publication-title: J. Korean Meteorol. Soc.
– volume: 19
  start-page: 5686
  year: 2006
  end-page: 5699
  article-title: Robust responses of the hydrological cycle to global warming
  publication-title: J. Climate
– ident: e_1_2_6_4_1
  doi: 10.1029/2009JD012008
– ident: e_1_2_6_10_1
  doi: 10.1038/ngeo262
– ident: e_1_2_6_12_1
  doi: 10.1029/2009GL040218
– volume: 42
  start-page: 129
  year: 2006
  ident: e_1_2_6_8_1
  article-title: The WRF single‐moment 6‐class microphysics scheme (WSM6)
  publication-title: J. Korean Meteorol. Soc.
– ident: e_1_2_6_18_1
  doi: 10.1029/2005GL022465
– ident: e_1_2_6_7_1
  doi: 10.1175/JCLI3990.1
– ident: e_1_2_6_11_1
  doi: 10.1088/1748-9326/5/2/025208
– ident: e_1_2_6_3_1
  doi: 10.1038/nature01092
– ident: e_1_2_6_14_1
  doi: 10.1007/s00382-006-0180-2
– ident: e_1_2_6_17_1
  doi: 10.1175/1520-0469(1988)045<1990:SAEONS>2.0.CO;2
– ident: e_1_2_6_9_1
  doi: 10.1029/2004RG000150
– ident: e_1_2_6_16_1
  doi: 10.1175/BAMS-84-9-1205
– ident: e_1_2_6_5_1
  doi: 10.1016/0022-1694(95)02953-2
– ident: e_1_2_6_2_1
  doi: 10.1029/1998WR900013
– ident: e_1_2_6_13_1
  doi: 10.1175/2009JCLI2701.1
– ident: e_1_2_6_15_1
– ident: e_1_2_6_6_1
  doi: 10.1038/ngeo523
SSID ssj0005727
Score 2.3501987
Snippet The sensitivity of squall rainfall to changes in atmospheric temperature is investigated. For instantaneous rainrates and accumulations up to one hour, extreme...
SourceID proquest
crossref
wiley
SourceType Aggregation Database
Enrichment Source
Index Database
Publisher
StartPage 334
SubjectTerms Accumulations
Atmospheric temperature
Clausius–Clapeyron scaling
Climate change
Copyrights
Design parameters
Extreme weather
Flooding
High temperature
PMP
probable maximum precipitation
Rainfall
rainfall extremes
Reproduction
Squalls
Title Super‐Clausius–Clapeyron scaling of rainfall in a model squall line
URI https://onlinelibrary.wiley.com/doi/abs/10.1002%2Fqj.1919
https://www.proquest.com/docview/1317620654
https://www.proquest.com/docview/1434018540
https://www.proquest.com/docview/1642248670
Volume 139
WOSCitedRecordID wos000316623700006&url=https%3A%2F%2Fcvtisr.summon.serialssolutions.com%2F%23%21%2Fsearch%3Fho%3Df%26include.ft.matches%3Dt%26l%3Dnull%26q%3D
hasFullText 1
inHoldings 1
isFullTextHit
isPrint
journalDatabaseRights – providerCode: PRVWIB
  databaseName: Wiley Online Library - Journals
  customDbUrl:
  eissn: 1477-870X
  dateEnd: 99991231
  omitProxy: false
  ssIdentifier: ssj0005727
  issn: 0035-9009
  databaseCode: DRFUL
  dateStart: 20020101
  isFulltext: true
  titleUrlDefault: https://onlinelibrary.wiley.com
  providerName: Wiley-Blackwell
link http://cvtisr.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwpV3fa9UwFA6y7WEvTufEO-eIMPZWZpImTR_l6lVkjqkb7K3kV-FCae_adeDb_gTB_3B_ieek3b2ToQhCoS09gZDk5HwnTb6PkANuJLe5yhPpckhQXNCJ4Y4luP1CyTIDBB7Z9Y-zkxN9cZGf3pP6Gvghlgtu6BlxvkYHN7Y7WpGGXoKX50j4uc6YyHBA8_R0tbsjG9VahUxywBHDeVksejQW_D0QrdDlfYwag8xs6z-q94Q8HpElfTsMhafkUai3yeQzgOKmjWvn9JBOqzkg1Pj2jHz41i9Ce3vzY1qZvpv33e3NT3hchO9tU9MOOg_CGm1KiioSpakqOq-poVE7h3Z4GrOiWM8dcj57fzb9mIy6ColLYYJKnBdBSYfMN0orKz1zzL7RVvlUhhJSQpFr7S1cSM3iASI4Hwz3TjhtlCvFc7JWN3V4QSjLhNQWUIL1PmVWGgiJxjBlU8uFl3ZCDu8auXAj6ThqX1TFQJfMi0vIPqCdJoQuDRcDz8ZDk727XipGR-sKBvhHcTwhOyGvl5_BRfC_h6lD04NNKiCL1IBN_2IDeRhH9kGwOYj9-qdqFF8-4W3338xekk0eBTRw0WaPrF21fXhFNtz11bxr9-OY3Sfr777Ozo9_AelP8W8
linkProvider Wiley-Blackwell
linkToHtml http://cvtisr.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwpV3batwwEB3CJtC-tE0vZNs0USHkzaSWLa38WLbdpOlm6SWBvBndDAvG3thxoW_5hED-MF_SGdvZbSkthYDBNh6BkDSaM2PNGYA9rgU3iUwCYRN0UKxXgeY2DOj4hRTZCBF4y64_Hc1m6vw8-dyfqqRcmI4fYhlwI81o92tScApIH6xYQy9QzRNi_FyPcRGJAay__zo5m64OeIz6gq2RCBKEEl3KLDU-6Jv-botWAPNXmNramcnj-_TwCTzq0SV71y2HTVjzxVMYniAwLqs2fs722TifI0pt357B4bdm4avbq-txrpt63tS3Vzf4uPA_qrJgNU4gmjZWZowqSWQ6z9m8YJq19XNYTRmZOaOOPoezyYfT8VHQ11YIbIybVGBd5KWwxH4jlTTChTY0b5WRLhY-Q7cwSpRyBi-iZ3EIE6zzmjsbWaWlzaIXMCjKwm8BC0eRUAaRgnEuDo3QaBa1DqWJDY-cMEPYvxvl1PbE41T_Ik87ymSeXqAHguM0BLYUXHRcG3-KbN9NU9orW52GiIEkpyzZIbxZfkY1oX8fuvBlgzJxhJ6kQnz6Dxn0xTgxEKLMXjuxf-tG-uWYbi__T2wXHhydnkzT6cfZp1fwkLcFNSiIsw2Dy6rxr2HDfr-c19VOv4R_AgtY9Uw
linkToPdf http://cvtisr.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwpV1fS9xAEF_EivhSq23pqdUtiG_BZpPd2zyWa8-_PU6q4FvYf4GDkJyJEXzzIwj9hn6SzmzinSItBSGQhMzCsLuz85vNzm8I2WWKM52IJOAmgQDFOBkoZsIAj18InvUBgXt2_dP-aCQvL5Nxd6oSc2FafojZhhtahl-v0cDd1Gb7c9bQKzDzBBk_38QcVlhkdY7H8-Md_a5ca8SDBIBEmzCLTfe7hs890RxePgWp3ssMV1-j3zvytsOW9Fs7GdbIgivWSe8nwOKy8rvndI8O8glgVP_2nhz8aqaueri7H-SqqSdN_XD3Gx6n7rYqC1rD8IFjo2VGsY5EpvKcTgqqqK-eQ2vMx8wpKvqBXAx_nA8Og66yQmBiWKICYyMnuEHuGyGF5jY0of4qtbAxdxkEhVEipdVwITmLBZBgrFPMmshIJUwWfSSLRVm4T4SG_YhLDThBWxuHmitwikqFQseaRZbrHtl77OXUdLTjWP0iT1vCZJZeQfwB_dQjdCY4bZk2XopsPQ5T2planYaAgATDHNke-TL7DEaCfz5U4coGZOII4kgJ6PQfMhCJMeQfBJldP7B_UyM9O8bbxv-J7ZDl8fdheno0OtkkK8xX08AdnC2yeF017jNZMjfXk7ra9vP3D0_c8zU
openUrl ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fsummon.serialssolutions.com&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.atitle=Super-Clausius-Clapeyron+scaling+of+rainfall+in+a+model+squall+line&rft.jtitle=Quarterly+journal+of+the+Royal+Meteorological+Society&rft.au=Singleton%2C+Andrew&rft.au=Toumi%2C+Ralf&rft.date=2013-01-01&rft.pub=Wiley+Subscription+Services%2C+Inc&rft.issn=0035-9009&rft.eissn=1477-870X&rft.volume=139&rft.issue=671+Part+B&rft.spage=334&rft_id=info:doi/10.1002%2Fqj.1919&rft.externalDBID=NO_FULL_TEXT&rft.externalDocID=2920817351
thumbnail_l http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/lc.gif&issn=0035-9009&client=summon
thumbnail_m http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/mc.gif&issn=0035-9009&client=summon
thumbnail_s http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/sc.gif&issn=0035-9009&client=summon