The characteristics of turbulent velocity components in the surface layer under convective conditions
Abstract It is proposed that the ratios of the standard deviations of the horizontal velocity components to the friction velocity in the surface layer under convective conditions depend only onzi/L wherezi is the height of the lowest inversion andL is the Monin-Obukhov length. This hypothesis is tes...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Panofsky, H. A. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1977 |
|---|
| Schlagwörter: |
|---|
| Anmerkung: |
© D. Reidel Publishing Company 1977 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Boundary layer meteorology - Kluwer Academic Publishers, 1970, 11(1977), 3 vom: Mai, Seite 355-361 |
|---|---|
| Übergeordnetes Werk: |
volume:11 ; year:1977 ; number:3 ; month:05 ; pages:355-361 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF02186086 |
|---|
| Katalog-ID: |
OLC2060920981 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | OLC2060920981 | ||
| 003 | DE-627 | ||
| 005 | 20230503004759.0 | ||
| 007 | tu | ||
| 008 | 200819s1977 xx ||||| 00| ||eng c | ||
| 024 | 7 | |a 10.1007/BF02186086 |2 doi | |
| 035 | |a (DE-627)OLC2060920981 | ||
| 035 | |a (DE-He213)BF02186086-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 Panofsky, H. A. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a The characteristics of turbulent velocity components in the surface layer under convective conditions |
| 264 | 1 | |c 1977 | |
| 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 © D. Reidel Publishing Company 1977 | ||
| 520 | |a Abstract It is proposed that the ratios of the standard deviations of the horizontal velocity components to the friction velocity in the surface layer under convective conditions depend only onzi/L wherezi is the height of the lowest inversion andL is the Monin-Obukhov length. This hypothesis is tested by using observations from several data sets over uniform surfaces and appears to fit the data well. Empirical curves are fitted to the observations which have the property that at largezi/-L, the standard deviations become proportional tow*, the convective scaling velocity. Fluctuations of vertical velocity obtained from the same experiments scale withz/L, wherez is the height above the surface, in good agreement with Monin-Obukhov theory. | ||
| 650 | 4 | |a Standard Deviation | |
| 650 | 4 | |a Surface Layer | |
| 650 | 4 | |a Velocity Component | |
| 650 | 4 | |a Vertical Velocity | |
| 650 | 4 | |a Horizontal Velocity | |
| 700 | 1 | |a Tennekes, H. |4 aut | |
| 700 | 1 | |a Lenschow, D. H. |4 aut | |
| 700 | 1 | |a Wyngaard, J. C. |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Boundary layer meteorology |d Kluwer Academic Publishers, 1970 |g 11(1977), 3 vom: Mai, Seite 355-361 |w (DE-627)129610410 |w (DE-600)242879-9 |w (DE-576)015105679 |x 0006-8314 |7 nnns |
| 773 | 1 | 8 | |g volume:11 |g year:1977 |g number:3 |g month:05 |g pages:355-361 |
| 856 | 4 | 1 | |u https://doi.org/10.1007/BF02186086 |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_11 | ||
| 912 | |a GBV_ILN_21 | ||
| 912 | |a GBV_ILN_22 | ||
| 912 | |a GBV_ILN_40 | ||
| 912 | |a GBV_ILN_47 | ||
| 912 | |a GBV_ILN_70 | ||
| 912 | |a GBV_ILN_154 | ||
| 912 | |a GBV_ILN_201 | ||
| 912 | |a GBV_ILN_601 | ||
| 912 | |a GBV_ILN_2006 | ||
| 912 | |a GBV_ILN_2010 | ||
| 912 | |a GBV_ILN_2012 | ||
| 912 | |a GBV_ILN_2014 | ||
| 912 | |a GBV_ILN_4012 | ||
| 912 | |a GBV_ILN_4305 | ||
| 912 | |a GBV_ILN_4307 | ||
| 912 | |a GBV_ILN_4311 | ||
| 951 | |a AR | ||
| 952 | |d 11 |j 1977 |e 3 |c 05 |h 355-361 | ||
| author_variant |
h a p ha hap h t ht d h l dh dhl j c w jc jcw |
|---|---|
| matchkey_str |
article:00068314:1977----::hcaatrsisfublnvlctcmoetiteufclyrn |
| hierarchy_sort_str |
1977 |
| publishDate |
1977 |
| allfields |
10.1007/BF02186086 doi (DE-627)OLC2060920981 (DE-He213)BF02186086-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Panofsky, H. A. verfasserin aut The characteristics of turbulent velocity components in the surface layer under convective conditions 1977 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1977 Abstract It is proposed that the ratios of the standard deviations of the horizontal velocity components to the friction velocity in the surface layer under convective conditions depend only onzi/L wherezi is the height of the lowest inversion andL is the Monin-Obukhov length. This hypothesis is tested by using observations from several data sets over uniform surfaces and appears to fit the data well. Empirical curves are fitted to the observations which have the property that at largezi/-L, the standard deviations become proportional tow*, the convective scaling velocity. Fluctuations of vertical velocity obtained from the same experiments scale withz/L, wherez is the height above the surface, in good agreement with Monin-Obukhov theory. Standard Deviation Surface Layer Velocity Component Vertical Velocity Horizontal Velocity Tennekes, H. aut Lenschow, D. H. aut Wyngaard, J. C. aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 11(1977), 3 vom: Mai, Seite 355-361 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:11 year:1977 number:3 month:05 pages:355-361 https://doi.org/10.1007/BF02186086 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_154 GBV_ILN_201 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2012 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4311 AR 11 1977 3 05 355-361 |
| spelling |
10.1007/BF02186086 doi (DE-627)OLC2060920981 (DE-He213)BF02186086-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Panofsky, H. A. verfasserin aut The characteristics of turbulent velocity components in the surface layer under convective conditions 1977 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1977 Abstract It is proposed that the ratios of the standard deviations of the horizontal velocity components to the friction velocity in the surface layer under convective conditions depend only onzi/L wherezi is the height of the lowest inversion andL is the Monin-Obukhov length. This hypothesis is tested by using observations from several data sets over uniform surfaces and appears to fit the data well. Empirical curves are fitted to the observations which have the property that at largezi/-L, the standard deviations become proportional tow*, the convective scaling velocity. Fluctuations of vertical velocity obtained from the same experiments scale withz/L, wherez is the height above the surface, in good agreement with Monin-Obukhov theory. Standard Deviation Surface Layer Velocity Component Vertical Velocity Horizontal Velocity Tennekes, H. aut Lenschow, D. H. aut Wyngaard, J. C. aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 11(1977), 3 vom: Mai, Seite 355-361 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:11 year:1977 number:3 month:05 pages:355-361 https://doi.org/10.1007/BF02186086 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_154 GBV_ILN_201 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2012 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4311 AR 11 1977 3 05 355-361 |
| allfields_unstemmed |
10.1007/BF02186086 doi (DE-627)OLC2060920981 (DE-He213)BF02186086-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Panofsky, H. A. verfasserin aut The characteristics of turbulent velocity components in the surface layer under convective conditions 1977 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1977 Abstract It is proposed that the ratios of the standard deviations of the horizontal velocity components to the friction velocity in the surface layer under convective conditions depend only onzi/L wherezi is the height of the lowest inversion andL is the Monin-Obukhov length. This hypothesis is tested by using observations from several data sets over uniform surfaces and appears to fit the data well. Empirical curves are fitted to the observations which have the property that at largezi/-L, the standard deviations become proportional tow*, the convective scaling velocity. Fluctuations of vertical velocity obtained from the same experiments scale withz/L, wherez is the height above the surface, in good agreement with Monin-Obukhov theory. Standard Deviation Surface Layer Velocity Component Vertical Velocity Horizontal Velocity Tennekes, H. aut Lenschow, D. H. aut Wyngaard, J. C. aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 11(1977), 3 vom: Mai, Seite 355-361 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:11 year:1977 number:3 month:05 pages:355-361 https://doi.org/10.1007/BF02186086 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_154 GBV_ILN_201 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2012 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4311 AR 11 1977 3 05 355-361 |
| allfieldsGer |
10.1007/BF02186086 doi (DE-627)OLC2060920981 (DE-He213)BF02186086-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Panofsky, H. A. verfasserin aut The characteristics of turbulent velocity components in the surface layer under convective conditions 1977 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1977 Abstract It is proposed that the ratios of the standard deviations of the horizontal velocity components to the friction velocity in the surface layer under convective conditions depend only onzi/L wherezi is the height of the lowest inversion andL is the Monin-Obukhov length. This hypothesis is tested by using observations from several data sets over uniform surfaces and appears to fit the data well. Empirical curves are fitted to the observations which have the property that at largezi/-L, the standard deviations become proportional tow*, the convective scaling velocity. Fluctuations of vertical velocity obtained from the same experiments scale withz/L, wherez is the height above the surface, in good agreement with Monin-Obukhov theory. Standard Deviation Surface Layer Velocity Component Vertical Velocity Horizontal Velocity Tennekes, H. aut Lenschow, D. H. aut Wyngaard, J. C. aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 11(1977), 3 vom: Mai, Seite 355-361 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:11 year:1977 number:3 month:05 pages:355-361 https://doi.org/10.1007/BF02186086 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_154 GBV_ILN_201 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2012 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4311 AR 11 1977 3 05 355-361 |
| allfieldsSound |
10.1007/BF02186086 doi (DE-627)OLC2060920981 (DE-He213)BF02186086-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Panofsky, H. A. verfasserin aut The characteristics of turbulent velocity components in the surface layer under convective conditions 1977 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1977 Abstract It is proposed that the ratios of the standard deviations of the horizontal velocity components to the friction velocity in the surface layer under convective conditions depend only onzi/L wherezi is the height of the lowest inversion andL is the Monin-Obukhov length. This hypothesis is tested by using observations from several data sets over uniform surfaces and appears to fit the data well. Empirical curves are fitted to the observations which have the property that at largezi/-L, the standard deviations become proportional tow*, the convective scaling velocity. Fluctuations of vertical velocity obtained from the same experiments scale withz/L, wherez is the height above the surface, in good agreement with Monin-Obukhov theory. Standard Deviation Surface Layer Velocity Component Vertical Velocity Horizontal Velocity Tennekes, H. aut Lenschow, D. H. aut Wyngaard, J. C. aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 11(1977), 3 vom: Mai, Seite 355-361 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:11 year:1977 number:3 month:05 pages:355-361 https://doi.org/10.1007/BF02186086 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_154 GBV_ILN_201 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2012 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4311 AR 11 1977 3 05 355-361 |
| language |
English |
| source |
Enthalten in Boundary layer meteorology 11(1977), 3 vom: Mai, Seite 355-361 volume:11 year:1977 number:3 month:05 pages:355-361 |
| sourceStr |
Enthalten in Boundary layer meteorology 11(1977), 3 vom: Mai, Seite 355-361 volume:11 year:1977 number:3 month:05 pages:355-361 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Standard Deviation Surface Layer Velocity Component Vertical Velocity Horizontal Velocity |
| dewey-raw |
550 |
| isfreeaccess_bool |
false |
| container_title |
Boundary layer meteorology |
| authorswithroles_txt_mv |
Panofsky, H. A. @@aut@@ Tennekes, H. @@aut@@ Lenschow, D. H. @@aut@@ Wyngaard, J. C. @@aut@@ |
| publishDateDaySort_date |
1977-05-01T00:00:00Z |
| hierarchy_top_id |
129610410 |
| dewey-sort |
3550 |
| id |
OLC2060920981 |
| 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">OLC2060920981</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230503004759.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s1977 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF02186086</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2060920981</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)BF02186086-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">Panofsky, H. A.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">The characteristics of turbulent velocity components in the surface layer under convective conditions</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1977</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">© D. Reidel Publishing Company 1977</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract It is proposed that the ratios of the standard deviations of the horizontal velocity components to the friction velocity in the surface layer under convective conditions depend only onzi/L wherezi is the height of the lowest inversion andL is the Monin-Obukhov length. This hypothesis is tested by using observations from several data sets over uniform surfaces and appears to fit the data well. Empirical curves are fitted to the observations which have the property that at largezi/-L, the standard deviations become proportional tow*, the convective scaling velocity. Fluctuations of vertical velocity obtained from the same experiments scale withz/L, wherez is the height above the surface, in good agreement with Monin-Obukhov theory.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Standard Deviation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Surface Layer</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Velocity Component</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Vertical Velocity</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Horizontal Velocity</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tennekes, H.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Lenschow, D. H.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wyngaard, J. C.</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">11(1977), 3 vom: Mai, Seite 355-361</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:11</subfield><subfield code="g">year:1977</subfield><subfield code="g">number:3</subfield><subfield code="g">month:05</subfield><subfield code="g">pages:355-361</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/BF02186086</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_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_21</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_47</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_201</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_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_2012</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_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4311</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">11</subfield><subfield code="j">1977</subfield><subfield code="e">3</subfield><subfield code="c">05</subfield><subfield code="h">355-361</subfield></datafield></record></collection>
|
| author |
Panofsky, H. A. |
| spellingShingle |
Panofsky, H. A. ddc 550 ssgn 16,13 misc Standard Deviation misc Surface Layer misc Velocity Component misc Vertical Velocity misc Horizontal Velocity The characteristics of turbulent velocity components in the surface layer under convective conditions |
| authorStr |
Panofsky, H. A. |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)129610410 |
| format |
Article |
| dewey-ones |
550 - Earth sciences |
| delete_txt_mv |
keep |
| author_role |
aut aut aut aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
0006-8314 |
| topic_title |
550 VZ 16,13 ssgn The characteristics of turbulent velocity components in the surface layer under convective conditions Standard Deviation Surface Layer Velocity Component Vertical Velocity Horizontal Velocity |
| topic |
ddc 550 ssgn 16,13 misc Standard Deviation misc Surface Layer misc Velocity Component misc Vertical Velocity misc Horizontal Velocity |
| topic_unstemmed |
ddc 550 ssgn 16,13 misc Standard Deviation misc Surface Layer misc Velocity Component misc Vertical Velocity misc Horizontal Velocity |
| topic_browse |
ddc 550 ssgn 16,13 misc Standard Deviation misc Surface Layer misc Velocity Component misc Vertical Velocity misc Horizontal Velocity |
| 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 |
The characteristics of turbulent velocity components in the surface layer under convective conditions |
| ctrlnum |
(DE-627)OLC2060920981 (DE-He213)BF02186086-p |
| title_full |
The characteristics of turbulent velocity components in the surface layer under convective conditions |
| author_sort |
Panofsky, H. A. |
| journal |
Boundary layer meteorology |
| journalStr |
Boundary layer meteorology |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| publishDateSort |
1977 |
| contenttype_str_mv |
txt |
| container_start_page |
355 |
| author_browse |
Panofsky, H. A. Tennekes, H. Lenschow, D. H. Wyngaard, J. C. |
| container_volume |
11 |
| class |
550 VZ 16,13 ssgn |
| format_se |
Aufsätze |
| author-letter |
Panofsky, H. A. |
| doi_str_mv |
10.1007/BF02186086 |
| dewey-full |
550 |
| title_sort |
the characteristics of turbulent velocity components in the surface layer under convective conditions |
| title_auth |
The characteristics of turbulent velocity components in the surface layer under convective conditions |
| abstract |
Abstract It is proposed that the ratios of the standard deviations of the horizontal velocity components to the friction velocity in the surface layer under convective conditions depend only onzi/L wherezi is the height of the lowest inversion andL is the Monin-Obukhov length. This hypothesis is tested by using observations from several data sets over uniform surfaces and appears to fit the data well. Empirical curves are fitted to the observations which have the property that at largezi/-L, the standard deviations become proportional tow*, the convective scaling velocity. Fluctuations of vertical velocity obtained from the same experiments scale withz/L, wherez is the height above the surface, in good agreement with Monin-Obukhov theory. © D. Reidel Publishing Company 1977 |
| abstractGer |
Abstract It is proposed that the ratios of the standard deviations of the horizontal velocity components to the friction velocity in the surface layer under convective conditions depend only onzi/L wherezi is the height of the lowest inversion andL is the Monin-Obukhov length. This hypothesis is tested by using observations from several data sets over uniform surfaces and appears to fit the data well. Empirical curves are fitted to the observations which have the property that at largezi/-L, the standard deviations become proportional tow*, the convective scaling velocity. Fluctuations of vertical velocity obtained from the same experiments scale withz/L, wherez is the height above the surface, in good agreement with Monin-Obukhov theory. © D. Reidel Publishing Company 1977 |
| abstract_unstemmed |
Abstract It is proposed that the ratios of the standard deviations of the horizontal velocity components to the friction velocity in the surface layer under convective conditions depend only onzi/L wherezi is the height of the lowest inversion andL is the Monin-Obukhov length. This hypothesis is tested by using observations from several data sets over uniform surfaces and appears to fit the data well. Empirical curves are fitted to the observations which have the property that at largezi/-L, the standard deviations become proportional tow*, the convective scaling velocity. Fluctuations of vertical velocity obtained from the same experiments scale withz/L, wherez is the height above the surface, in good agreement with Monin-Obukhov theory. © D. Reidel Publishing Company 1977 |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_154 GBV_ILN_201 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2012 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4311 |
| container_issue |
3 |
| title_short |
The characteristics of turbulent velocity components in the surface layer under convective conditions |
| url |
https://doi.org/10.1007/BF02186086 |
| remote_bool |
false |
| author2 |
Tennekes, H. Lenschow, D. H. Wyngaard, J. C. |
| author2Str |
Tennekes, H. Lenschow, D. H. Wyngaard, J. C. |
| ppnlink |
129610410 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1007/BF02186086 |
| up_date |
2024-07-04T02:26:52.108Z |
| _version_ |
1803613647259303936 |
| 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">OLC2060920981</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230503004759.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s1977 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF02186086</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2060920981</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)BF02186086-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">Panofsky, H. A.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">The characteristics of turbulent velocity components in the surface layer under convective conditions</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1977</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">© D. Reidel Publishing Company 1977</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract It is proposed that the ratios of the standard deviations of the horizontal velocity components to the friction velocity in the surface layer under convective conditions depend only onzi/L wherezi is the height of the lowest inversion andL is the Monin-Obukhov length. This hypothesis is tested by using observations from several data sets over uniform surfaces and appears to fit the data well. Empirical curves are fitted to the observations which have the property that at largezi/-L, the standard deviations become proportional tow*, the convective scaling velocity. Fluctuations of vertical velocity obtained from the same experiments scale withz/L, wherez is the height above the surface, in good agreement with Monin-Obukhov theory.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Standard Deviation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Surface Layer</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Velocity Component</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Vertical Velocity</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Horizontal Velocity</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tennekes, H.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Lenschow, D. H.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wyngaard, J. C.</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">11(1977), 3 vom: Mai, Seite 355-361</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:11</subfield><subfield code="g">year:1977</subfield><subfield code="g">number:3</subfield><subfield code="g">month:05</subfield><subfield code="g">pages:355-361</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/BF02186086</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_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_21</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_47</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_201</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_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_2012</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_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4311</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">11</subfield><subfield code="j">1977</subfield><subfield code="e">3</subfield><subfield code="c">05</subfield><subfield code="h">355-361</subfield></datafield></record></collection>
|
| score |
7.3993683 |