Do stratocumulus clouds detrain? FIRE I data revisited
Abstract Analyses of aircraft observations of the stratocumulus-topped boundary layer during the First ISCCP (International Satellite Cloud Climatology Project) Regional Experiment (FIRE I) show the frequent presence of clear, but relatively moist, air patches near the stratocumulus cloud-top interf...
Ausführliche Beschreibung
Autor*in: |
de Roode, Stephan R. [verfasserIn] |
---|
Format: |
Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
2006 |
---|
Schlagwörter: |
---|
Anmerkung: |
© Springer Science+Business Media M.V 2006 |
---|
Übergeordnetes Werk: |
Enthalten in: Boundary layer meteorology - Kluwer Academic Publishers, 1970, 122(2006), 2 vom: 19. Okt., Seite 479-491 |
---|---|
Übergeordnetes Werk: |
volume:122 ; year:2006 ; number:2 ; day:19 ; month:10 ; pages:479-491 |
Links: |
---|
DOI / URN: |
10.1007/s10546-006-9113-1 |
---|
Katalog-ID: |
OLC2060952263 |
---|
LEADER | 01000caa a22002652 4500 | ||
---|---|---|---|
001 | OLC2060952263 | ||
003 | DE-627 | ||
005 | 20230503005006.0 | ||
007 | tu | ||
008 | 200819s2006 xx ||||| 00| ||eng c | ||
024 | 7 | |a 10.1007/s10546-006-9113-1 |2 doi | |
035 | |a (DE-627)OLC2060952263 | ||
035 | |a (DE-He213)s10546-006-9113-1-p | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
082 | 0 | 4 | |a 550 |q VZ |
084 | |a 16,13 |2 ssgn | ||
100 | 1 | |a de Roode, Stephan R. |e verfasserin |4 aut | |
245 | 1 | 0 | |a Do stratocumulus clouds detrain? FIRE I data revisited |
264 | 1 | |c 2006 | |
336 | |a Text |b txt |2 rdacontent | ||
337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
338 | |a Band |b nc |2 rdacarrier | ||
500 | |a © Springer Science+Business Media M.V 2006 | ||
520 | |a Abstract Analyses of aircraft observations of the stratocumulus-topped boundary layer during the First ISCCP (International Satellite Cloud Climatology Project) Regional Experiment (FIRE I) show the frequent presence of clear, but relatively moist, air patches near the stratocumulus cloud-top interface. A conditional sampling of measurements in these clear air patches shows that their thermodynamic properties do more resemble boundary-layer air characteristics than those of free troposphere air. From an aircraft leg through cloud tops it is demonstrated that turbulent mixing across the cloud-top interface can lead to the local dissipation of the cloud top. Analogous to the terminology used for shallow cumulus parameterizations this process can be considered as detrainment, with which we mean that after a mixing event across the cloud-top boundaries, mixed unsaturated parcels become part of the clear environment of the cloud. | ||
650 | 4 | |a Aircraft observations | |
650 | 4 | |a Boundary-layer clouds | |
650 | 4 | |a Conditional sampling | |
650 | 4 | |a FIRE I | |
650 | 4 | |a ISCCP | |
650 | 4 | |a Inversion structure | |
650 | 4 | |a Stratocumulus | |
700 | 1 | |a Wang, Qing |4 aut | |
773 | 0 | 8 | |i Enthalten in |t Boundary layer meteorology |d Kluwer Academic Publishers, 1970 |g 122(2006), 2 vom: 19. Okt., Seite 479-491 |w (DE-627)129610410 |w (DE-600)242879-9 |w (DE-576)015105679 |x 0006-8314 |7 nnns |
773 | 1 | 8 | |g volume:122 |g year:2006 |g number:2 |g day:19 |g month:10 |g pages:479-491 |
856 | 4 | 1 | |u https://doi.org/10.1007/s10546-006-9113-1 |z lizenzpflichtig |3 Volltext |
912 | |a GBV_USEFLAG_A | ||
912 | |a SYSFLAG_A | ||
912 | |a GBV_OLC | ||
912 | |a SSG-OLC-GEO | ||
912 | |a SSG-OPC-GGO | ||
912 | |a SSG-OPC-GEO | ||
912 | |a GBV_ILN_22 | ||
912 | |a GBV_ILN_40 | ||
912 | |a GBV_ILN_70 | ||
912 | |a GBV_ILN_154 | ||
912 | |a GBV_ILN_381 | ||
912 | |a GBV_ILN_601 | ||
912 | |a GBV_ILN_602 | ||
912 | |a GBV_ILN_2003 | ||
912 | |a GBV_ILN_2006 | ||
912 | |a GBV_ILN_2010 | ||
912 | |a GBV_ILN_2014 | ||
912 | |a GBV_ILN_4305 | ||
951 | |a AR | ||
952 | |d 122 |j 2006 |e 2 |b 19 |c 10 |h 479-491 |
author_variant |
r s r d rsr rsrd q w qw |
---|---|
matchkey_str |
article:00068314:2006----::otaouuucoddtanie |
hierarchy_sort_str |
2006 |
publishDate |
2006 |
allfields |
10.1007/s10546-006-9113-1 doi (DE-627)OLC2060952263 (DE-He213)s10546-006-9113-1-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn de Roode, Stephan R. verfasserin aut Do stratocumulus clouds detrain? FIRE I data revisited 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media M.V 2006 Abstract Analyses of aircraft observations of the stratocumulus-topped boundary layer during the First ISCCP (International Satellite Cloud Climatology Project) Regional Experiment (FIRE I) show the frequent presence of clear, but relatively moist, air patches near the stratocumulus cloud-top interface. A conditional sampling of measurements in these clear air patches shows that their thermodynamic properties do more resemble boundary-layer air characteristics than those of free troposphere air. From an aircraft leg through cloud tops it is demonstrated that turbulent mixing across the cloud-top interface can lead to the local dissipation of the cloud top. Analogous to the terminology used for shallow cumulus parameterizations this process can be considered as detrainment, with which we mean that after a mixing event across the cloud-top boundaries, mixed unsaturated parcels become part of the clear environment of the cloud. Aircraft observations Boundary-layer clouds Conditional sampling FIRE I ISCCP Inversion structure Stratocumulus Wang, Qing aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 122(2006), 2 vom: 19. Okt., Seite 479-491 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:122 year:2006 number:2 day:19 month:10 pages:479-491 https://doi.org/10.1007/s10546-006-9113-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_154 GBV_ILN_381 GBV_ILN_601 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_4305 AR 122 2006 2 19 10 479-491 |
spelling |
10.1007/s10546-006-9113-1 doi (DE-627)OLC2060952263 (DE-He213)s10546-006-9113-1-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn de Roode, Stephan R. verfasserin aut Do stratocumulus clouds detrain? FIRE I data revisited 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media M.V 2006 Abstract Analyses of aircraft observations of the stratocumulus-topped boundary layer during the First ISCCP (International Satellite Cloud Climatology Project) Regional Experiment (FIRE I) show the frequent presence of clear, but relatively moist, air patches near the stratocumulus cloud-top interface. A conditional sampling of measurements in these clear air patches shows that their thermodynamic properties do more resemble boundary-layer air characteristics than those of free troposphere air. From an aircraft leg through cloud tops it is demonstrated that turbulent mixing across the cloud-top interface can lead to the local dissipation of the cloud top. Analogous to the terminology used for shallow cumulus parameterizations this process can be considered as detrainment, with which we mean that after a mixing event across the cloud-top boundaries, mixed unsaturated parcels become part of the clear environment of the cloud. Aircraft observations Boundary-layer clouds Conditional sampling FIRE I ISCCP Inversion structure Stratocumulus Wang, Qing aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 122(2006), 2 vom: 19. Okt., Seite 479-491 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:122 year:2006 number:2 day:19 month:10 pages:479-491 https://doi.org/10.1007/s10546-006-9113-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_154 GBV_ILN_381 GBV_ILN_601 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_4305 AR 122 2006 2 19 10 479-491 |
allfields_unstemmed |
10.1007/s10546-006-9113-1 doi (DE-627)OLC2060952263 (DE-He213)s10546-006-9113-1-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn de Roode, Stephan R. verfasserin aut Do stratocumulus clouds detrain? FIRE I data revisited 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media M.V 2006 Abstract Analyses of aircraft observations of the stratocumulus-topped boundary layer during the First ISCCP (International Satellite Cloud Climatology Project) Regional Experiment (FIRE I) show the frequent presence of clear, but relatively moist, air patches near the stratocumulus cloud-top interface. A conditional sampling of measurements in these clear air patches shows that their thermodynamic properties do more resemble boundary-layer air characteristics than those of free troposphere air. From an aircraft leg through cloud tops it is demonstrated that turbulent mixing across the cloud-top interface can lead to the local dissipation of the cloud top. Analogous to the terminology used for shallow cumulus parameterizations this process can be considered as detrainment, with which we mean that after a mixing event across the cloud-top boundaries, mixed unsaturated parcels become part of the clear environment of the cloud. Aircraft observations Boundary-layer clouds Conditional sampling FIRE I ISCCP Inversion structure Stratocumulus Wang, Qing aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 122(2006), 2 vom: 19. Okt., Seite 479-491 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:122 year:2006 number:2 day:19 month:10 pages:479-491 https://doi.org/10.1007/s10546-006-9113-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_154 GBV_ILN_381 GBV_ILN_601 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_4305 AR 122 2006 2 19 10 479-491 |
allfieldsGer |
10.1007/s10546-006-9113-1 doi (DE-627)OLC2060952263 (DE-He213)s10546-006-9113-1-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn de Roode, Stephan R. verfasserin aut Do stratocumulus clouds detrain? FIRE I data revisited 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media M.V 2006 Abstract Analyses of aircraft observations of the stratocumulus-topped boundary layer during the First ISCCP (International Satellite Cloud Climatology Project) Regional Experiment (FIRE I) show the frequent presence of clear, but relatively moist, air patches near the stratocumulus cloud-top interface. A conditional sampling of measurements in these clear air patches shows that their thermodynamic properties do more resemble boundary-layer air characteristics than those of free troposphere air. From an aircraft leg through cloud tops it is demonstrated that turbulent mixing across the cloud-top interface can lead to the local dissipation of the cloud top. Analogous to the terminology used for shallow cumulus parameterizations this process can be considered as detrainment, with which we mean that after a mixing event across the cloud-top boundaries, mixed unsaturated parcels become part of the clear environment of the cloud. Aircraft observations Boundary-layer clouds Conditional sampling FIRE I ISCCP Inversion structure Stratocumulus Wang, Qing aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 122(2006), 2 vom: 19. Okt., Seite 479-491 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:122 year:2006 number:2 day:19 month:10 pages:479-491 https://doi.org/10.1007/s10546-006-9113-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_154 GBV_ILN_381 GBV_ILN_601 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_4305 AR 122 2006 2 19 10 479-491 |
allfieldsSound |
10.1007/s10546-006-9113-1 doi (DE-627)OLC2060952263 (DE-He213)s10546-006-9113-1-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn de Roode, Stephan R. verfasserin aut Do stratocumulus clouds detrain? FIRE I data revisited 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media M.V 2006 Abstract Analyses of aircraft observations of the stratocumulus-topped boundary layer during the First ISCCP (International Satellite Cloud Climatology Project) Regional Experiment (FIRE I) show the frequent presence of clear, but relatively moist, air patches near the stratocumulus cloud-top interface. A conditional sampling of measurements in these clear air patches shows that their thermodynamic properties do more resemble boundary-layer air characteristics than those of free troposphere air. From an aircraft leg through cloud tops it is demonstrated that turbulent mixing across the cloud-top interface can lead to the local dissipation of the cloud top. Analogous to the terminology used for shallow cumulus parameterizations this process can be considered as detrainment, with which we mean that after a mixing event across the cloud-top boundaries, mixed unsaturated parcels become part of the clear environment of the cloud. Aircraft observations Boundary-layer clouds Conditional sampling FIRE I ISCCP Inversion structure Stratocumulus Wang, Qing aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 122(2006), 2 vom: 19. Okt., Seite 479-491 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:122 year:2006 number:2 day:19 month:10 pages:479-491 https://doi.org/10.1007/s10546-006-9113-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_154 GBV_ILN_381 GBV_ILN_601 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_4305 AR 122 2006 2 19 10 479-491 |
language |
English |
source |
Enthalten in Boundary layer meteorology 122(2006), 2 vom: 19. Okt., Seite 479-491 volume:122 year:2006 number:2 day:19 month:10 pages:479-491 |
sourceStr |
Enthalten in Boundary layer meteorology 122(2006), 2 vom: 19. Okt., Seite 479-491 volume:122 year:2006 number:2 day:19 month:10 pages:479-491 |
format_phy_str_mv |
Article |
institution |
findex.gbv.de |
topic_facet |
Aircraft observations Boundary-layer clouds Conditional sampling FIRE I ISCCP Inversion structure Stratocumulus |
dewey-raw |
550 |
isfreeaccess_bool |
false |
container_title |
Boundary layer meteorology |
authorswithroles_txt_mv |
de Roode, Stephan R. @@aut@@ Wang, Qing @@aut@@ |
publishDateDaySort_date |
2006-10-19T00:00:00Z |
hierarchy_top_id |
129610410 |
dewey-sort |
3550 |
id |
OLC2060952263 |
language_de |
englisch |
fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2060952263</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230503005006.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2006 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10546-006-9113-1</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2060952263</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s10546-006-9113-1-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">16,13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">de Roode, Stephan R.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Do stratocumulus clouds detrain? FIRE I data revisited</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2006</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer Science+Business Media M.V 2006</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Analyses of aircraft observations of the stratocumulus-topped boundary layer during the First ISCCP (International Satellite Cloud Climatology Project) Regional Experiment (FIRE I) show the frequent presence of clear, but relatively moist, air patches near the stratocumulus cloud-top interface. A conditional sampling of measurements in these clear air patches shows that their thermodynamic properties do more resemble boundary-layer air characteristics than those of free troposphere air. From an aircraft leg through cloud tops it is demonstrated that turbulent mixing across the cloud-top interface can lead to the local dissipation of the cloud top. Analogous to the terminology used for shallow cumulus parameterizations this process can be considered as detrainment, with which we mean that after a mixing event across the cloud-top boundaries, mixed unsaturated parcels become part of the clear environment of the cloud.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Aircraft observations</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Boundary-layer clouds</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Conditional sampling</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">FIRE I</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">ISCCP</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Inversion structure</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Stratocumulus</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wang, Qing</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Boundary layer meteorology</subfield><subfield code="d">Kluwer Academic Publishers, 1970</subfield><subfield code="g">122(2006), 2 vom: 19. Okt., Seite 479-491</subfield><subfield code="w">(DE-627)129610410</subfield><subfield code="w">(DE-600)242879-9</subfield><subfield code="w">(DE-576)015105679</subfield><subfield code="x">0006-8314</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:122</subfield><subfield code="g">year:2006</subfield><subfield code="g">number:2</subfield><subfield code="g">day:19</subfield><subfield code="g">month:10</subfield><subfield code="g">pages:479-491</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s10546-006-9113-1</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_154</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_381</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_601</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2006</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">122</subfield><subfield code="j">2006</subfield><subfield code="e">2</subfield><subfield code="b">19</subfield><subfield code="c">10</subfield><subfield code="h">479-491</subfield></datafield></record></collection>
|
author |
de Roode, Stephan R. |
spellingShingle |
de Roode, Stephan R. ddc 550 ssgn 16,13 misc Aircraft observations misc Boundary-layer clouds misc Conditional sampling misc FIRE I misc ISCCP misc Inversion structure misc Stratocumulus Do stratocumulus clouds detrain? FIRE I data revisited |
authorStr |
de Roode, Stephan R. |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)129610410 |
format |
Article |
dewey-ones |
550 - Earth sciences |
delete_txt_mv |
keep |
author_role |
aut aut |
collection |
OLC |
remote_str |
false |
illustrated |
Not Illustrated |
issn |
0006-8314 |
topic_title |
550 VZ 16,13 ssgn Do stratocumulus clouds detrain? FIRE I data revisited Aircraft observations Boundary-layer clouds Conditional sampling FIRE I ISCCP Inversion structure Stratocumulus |
topic |
ddc 550 ssgn 16,13 misc Aircraft observations misc Boundary-layer clouds misc Conditional sampling misc FIRE I misc ISCCP misc Inversion structure misc Stratocumulus |
topic_unstemmed |
ddc 550 ssgn 16,13 misc Aircraft observations misc Boundary-layer clouds misc Conditional sampling misc FIRE I misc ISCCP misc Inversion structure misc Stratocumulus |
topic_browse |
ddc 550 ssgn 16,13 misc Aircraft observations misc Boundary-layer clouds misc Conditional sampling misc FIRE I misc ISCCP misc Inversion structure misc Stratocumulus |
format_facet |
Aufsätze Gedruckte Aufsätze |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
nc |
hierarchy_parent_title |
Boundary layer meteorology |
hierarchy_parent_id |
129610410 |
dewey-tens |
550 - Earth sciences & geology |
hierarchy_top_title |
Boundary layer meteorology |
isfreeaccess_txt |
false |
familylinks_str_mv |
(DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 |
title |
Do stratocumulus clouds detrain? FIRE I data revisited |
ctrlnum |
(DE-627)OLC2060952263 (DE-He213)s10546-006-9113-1-p |
title_full |
Do stratocumulus clouds detrain? FIRE I data revisited |
author_sort |
de Roode, Stephan R. |
journal |
Boundary layer meteorology |
journalStr |
Boundary layer meteorology |
lang_code |
eng |
isOA_bool |
false |
dewey-hundreds |
500 - Science |
recordtype |
marc |
publishDateSort |
2006 |
contenttype_str_mv |
txt |
container_start_page |
479 |
author_browse |
de Roode, Stephan R. Wang, Qing |
container_volume |
122 |
class |
550 VZ 16,13 ssgn |
format_se |
Aufsätze |
author-letter |
de Roode, Stephan R. |
doi_str_mv |
10.1007/s10546-006-9113-1 |
dewey-full |
550 |
title_sort |
do stratocumulus clouds detrain? fire i data revisited |
title_auth |
Do stratocumulus clouds detrain? FIRE I data revisited |
abstract |
Abstract Analyses of aircraft observations of the stratocumulus-topped boundary layer during the First ISCCP (International Satellite Cloud Climatology Project) Regional Experiment (FIRE I) show the frequent presence of clear, but relatively moist, air patches near the stratocumulus cloud-top interface. A conditional sampling of measurements in these clear air patches shows that their thermodynamic properties do more resemble boundary-layer air characteristics than those of free troposphere air. From an aircraft leg through cloud tops it is demonstrated that turbulent mixing across the cloud-top interface can lead to the local dissipation of the cloud top. Analogous to the terminology used for shallow cumulus parameterizations this process can be considered as detrainment, with which we mean that after a mixing event across the cloud-top boundaries, mixed unsaturated parcels become part of the clear environment of the cloud. © Springer Science+Business Media M.V 2006 |
abstractGer |
Abstract Analyses of aircraft observations of the stratocumulus-topped boundary layer during the First ISCCP (International Satellite Cloud Climatology Project) Regional Experiment (FIRE I) show the frequent presence of clear, but relatively moist, air patches near the stratocumulus cloud-top interface. A conditional sampling of measurements in these clear air patches shows that their thermodynamic properties do more resemble boundary-layer air characteristics than those of free troposphere air. From an aircraft leg through cloud tops it is demonstrated that turbulent mixing across the cloud-top interface can lead to the local dissipation of the cloud top. Analogous to the terminology used for shallow cumulus parameterizations this process can be considered as detrainment, with which we mean that after a mixing event across the cloud-top boundaries, mixed unsaturated parcels become part of the clear environment of the cloud. © Springer Science+Business Media M.V 2006 |
abstract_unstemmed |
Abstract Analyses of aircraft observations of the stratocumulus-topped boundary layer during the First ISCCP (International Satellite Cloud Climatology Project) Regional Experiment (FIRE I) show the frequent presence of clear, but relatively moist, air patches near the stratocumulus cloud-top interface. A conditional sampling of measurements in these clear air patches shows that their thermodynamic properties do more resemble boundary-layer air characteristics than those of free troposphere air. From an aircraft leg through cloud tops it is demonstrated that turbulent mixing across the cloud-top interface can lead to the local dissipation of the cloud top. Analogous to the terminology used for shallow cumulus parameterizations this process can be considered as detrainment, with which we mean that after a mixing event across the cloud-top boundaries, mixed unsaturated parcels become part of the clear environment of the cloud. © Springer Science+Business Media M.V 2006 |
collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_154 GBV_ILN_381 GBV_ILN_601 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_4305 |
container_issue |
2 |
title_short |
Do stratocumulus clouds detrain? FIRE I data revisited |
url |
https://doi.org/10.1007/s10546-006-9113-1 |
remote_bool |
false |
author2 |
Wang, Qing |
author2Str |
Wang, Qing |
ppnlink |
129610410 |
mediatype_str_mv |
n |
isOA_txt |
false |
hochschulschrift_bool |
false |
doi_str |
10.1007/s10546-006-9113-1 |
up_date |
2024-07-04T02:30:56.347Z |
_version_ |
1803613903362457600 |
fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2060952263</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230503005006.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2006 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10546-006-9113-1</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2060952263</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s10546-006-9113-1-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">16,13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">de Roode, Stephan R.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Do stratocumulus clouds detrain? FIRE I data revisited</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2006</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer Science+Business Media M.V 2006</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Analyses of aircraft observations of the stratocumulus-topped boundary layer during the First ISCCP (International Satellite Cloud Climatology Project) Regional Experiment (FIRE I) show the frequent presence of clear, but relatively moist, air patches near the stratocumulus cloud-top interface. A conditional sampling of measurements in these clear air patches shows that their thermodynamic properties do more resemble boundary-layer air characteristics than those of free troposphere air. From an aircraft leg through cloud tops it is demonstrated that turbulent mixing across the cloud-top interface can lead to the local dissipation of the cloud top. Analogous to the terminology used for shallow cumulus parameterizations this process can be considered as detrainment, with which we mean that after a mixing event across the cloud-top boundaries, mixed unsaturated parcels become part of the clear environment of the cloud.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Aircraft observations</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Boundary-layer clouds</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Conditional sampling</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">FIRE I</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">ISCCP</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Inversion structure</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Stratocumulus</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wang, Qing</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Boundary layer meteorology</subfield><subfield code="d">Kluwer Academic Publishers, 1970</subfield><subfield code="g">122(2006), 2 vom: 19. Okt., Seite 479-491</subfield><subfield code="w">(DE-627)129610410</subfield><subfield code="w">(DE-600)242879-9</subfield><subfield code="w">(DE-576)015105679</subfield><subfield code="x">0006-8314</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:122</subfield><subfield code="g">year:2006</subfield><subfield code="g">number:2</subfield><subfield code="g">day:19</subfield><subfield code="g">month:10</subfield><subfield code="g">pages:479-491</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s10546-006-9113-1</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_154</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_381</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_601</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2006</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">122</subfield><subfield code="j">2006</subfield><subfield code="e">2</subfield><subfield code="b">19</subfield><subfield code="c">10</subfield><subfield code="h">479-491</subfield></datafield></record></collection>
|
score |
7.400589 |