Characteristics of horizontal macroturbulence due to the currents in the Baltic Sea
Summary On the basis of current measurements in a number of sites in the southeastern and central Baltic, the following parameters of horizontal turbulence were estimated: components of turbulence intensity, moments of the correlation matrix, horizontal eddy-viscosity coefficients and directions of...
Ausführliche Beschreibung
Autor*in: |
Jankowski, Andrzej [verfasserIn] Catewicz, Zygmunt [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
1984 |
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Schlagwörter: |
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Anmerkung: |
© Deutsches Hydrographisches Institut 1984 |
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Übergeordnetes Werk: |
Enthalten in: Deutsche Hydrografische Zeitschrift - Loviscach, Jörn, Springer Berlin Heidelberg, 2011, 37(1984), 5 vom: Sept., Seite 173-200 |
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Übergeordnetes Werk: |
volume:37 ; year:1984 ; number:5 ; month:09 ; pages:173-200 |
Links: |
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DOI / URN: |
10.1007/BF02226971 |
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SPR055730604 |
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10.1007/BF02226971 doi (DE-627)SPR055730604 (SPR)BF02226971-e DE-627 ger DE-627 rakwb eng Jankowski, Andrzej verfasserin aut Characteristics of horizontal macroturbulence due to the currents in the Baltic Sea 1984 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Deutsches Hydrographisches Institut 1984 Summary On the basis of current measurements in a number of sites in the southeastern and central Baltic, the following parameters of horizontal turbulence were estimated: components of turbulence intensity, moments of the correlation matrix, horizontal eddy-viscosity coefficients and directions of the extreme exchange in the horizontal plane. The exchange coefficients were calculated by the Ertel method. Exemplary empirical probability distribution (histograms) of the pulsations of current velocity components and the power spectra were shown. Changes in the turbulence parameters, depending upon the temporal scale the measure of which was assumed to be the averaging period of a cosine filter, were analysed. The influence of inertial oscillations upon the magnitudes of horizontal turbulence characteristics was shown. Power Spectrum (dpeaa)DE-He213 Current Velocity (dpeaa)DE-He213 Turbulence Intensity (dpeaa)DE-He213 Empirical Probability (dpeaa)DE-He213 Current Measurement (dpeaa)DE-He213 Catewicz, Zygmunt verfasserin aut Enthalten in Loviscach, Jörn Deutsche Hydrografische Zeitschrift Springer Berlin Heidelberg, 2011 37(1984), 5 vom: Sept., Seite 173-200 1 Online-Ressource (21 MB, 00:25:44:00) (DE-627)1820839486 nnnm volume:37 year:1984 number:5 month:09 pages:173-200 https://dx.doi.org/10.1007/BF02226971 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER GBV_ILN_23 GBV_ILN_30 GBV_ILN_63 GBV_ILN_118 GBV_ILN_122 GBV_ILN_140 GBV_ILN_264 GBV_ILN_2057 GBV_ILN_2403 AR 37 1984 5 09 173-200 |
spelling |
10.1007/BF02226971 doi (DE-627)SPR055730604 (SPR)BF02226971-e DE-627 ger DE-627 rakwb eng Jankowski, Andrzej verfasserin aut Characteristics of horizontal macroturbulence due to the currents in the Baltic Sea 1984 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Deutsches Hydrographisches Institut 1984 Summary On the basis of current measurements in a number of sites in the southeastern and central Baltic, the following parameters of horizontal turbulence were estimated: components of turbulence intensity, moments of the correlation matrix, horizontal eddy-viscosity coefficients and directions of the extreme exchange in the horizontal plane. The exchange coefficients were calculated by the Ertel method. Exemplary empirical probability distribution (histograms) of the pulsations of current velocity components and the power spectra were shown. Changes in the turbulence parameters, depending upon the temporal scale the measure of which was assumed to be the averaging period of a cosine filter, were analysed. The influence of inertial oscillations upon the magnitudes of horizontal turbulence characteristics was shown. Power Spectrum (dpeaa)DE-He213 Current Velocity (dpeaa)DE-He213 Turbulence Intensity (dpeaa)DE-He213 Empirical Probability (dpeaa)DE-He213 Current Measurement (dpeaa)DE-He213 Catewicz, Zygmunt verfasserin aut Enthalten in Loviscach, Jörn Deutsche Hydrografische Zeitschrift Springer Berlin Heidelberg, 2011 37(1984), 5 vom: Sept., Seite 173-200 1 Online-Ressource (21 MB, 00:25:44:00) (DE-627)1820839486 nnnm volume:37 year:1984 number:5 month:09 pages:173-200 https://dx.doi.org/10.1007/BF02226971 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER GBV_ILN_23 GBV_ILN_30 GBV_ILN_63 GBV_ILN_118 GBV_ILN_122 GBV_ILN_140 GBV_ILN_264 GBV_ILN_2057 GBV_ILN_2403 AR 37 1984 5 09 173-200 |
allfields_unstemmed |
10.1007/BF02226971 doi (DE-627)SPR055730604 (SPR)BF02226971-e DE-627 ger DE-627 rakwb eng Jankowski, Andrzej verfasserin aut Characteristics of horizontal macroturbulence due to the currents in the Baltic Sea 1984 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Deutsches Hydrographisches Institut 1984 Summary On the basis of current measurements in a number of sites in the southeastern and central Baltic, the following parameters of horizontal turbulence were estimated: components of turbulence intensity, moments of the correlation matrix, horizontal eddy-viscosity coefficients and directions of the extreme exchange in the horizontal plane. The exchange coefficients were calculated by the Ertel method. Exemplary empirical probability distribution (histograms) of the pulsations of current velocity components and the power spectra were shown. Changes in the turbulence parameters, depending upon the temporal scale the measure of which was assumed to be the averaging period of a cosine filter, were analysed. The influence of inertial oscillations upon the magnitudes of horizontal turbulence characteristics was shown. Power Spectrum (dpeaa)DE-He213 Current Velocity (dpeaa)DE-He213 Turbulence Intensity (dpeaa)DE-He213 Empirical Probability (dpeaa)DE-He213 Current Measurement (dpeaa)DE-He213 Catewicz, Zygmunt verfasserin aut Enthalten in Loviscach, Jörn Deutsche Hydrografische Zeitschrift Springer Berlin Heidelberg, 2011 37(1984), 5 vom: Sept., Seite 173-200 1 Online-Ressource (21 MB, 00:25:44:00) (DE-627)1820839486 nnnm volume:37 year:1984 number:5 month:09 pages:173-200 https://dx.doi.org/10.1007/BF02226971 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER GBV_ILN_23 GBV_ILN_30 GBV_ILN_63 GBV_ILN_118 GBV_ILN_122 GBV_ILN_140 GBV_ILN_264 GBV_ILN_2057 GBV_ILN_2403 AR 37 1984 5 09 173-200 |
allfieldsGer |
10.1007/BF02226971 doi (DE-627)SPR055730604 (SPR)BF02226971-e DE-627 ger DE-627 rakwb eng Jankowski, Andrzej verfasserin aut Characteristics of horizontal macroturbulence due to the currents in the Baltic Sea 1984 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Deutsches Hydrographisches Institut 1984 Summary On the basis of current measurements in a number of sites in the southeastern and central Baltic, the following parameters of horizontal turbulence were estimated: components of turbulence intensity, moments of the correlation matrix, horizontal eddy-viscosity coefficients and directions of the extreme exchange in the horizontal plane. The exchange coefficients were calculated by the Ertel method. Exemplary empirical probability distribution (histograms) of the pulsations of current velocity components and the power spectra were shown. Changes in the turbulence parameters, depending upon the temporal scale the measure of which was assumed to be the averaging period of a cosine filter, were analysed. The influence of inertial oscillations upon the magnitudes of horizontal turbulence characteristics was shown. Power Spectrum (dpeaa)DE-He213 Current Velocity (dpeaa)DE-He213 Turbulence Intensity (dpeaa)DE-He213 Empirical Probability (dpeaa)DE-He213 Current Measurement (dpeaa)DE-He213 Catewicz, Zygmunt verfasserin aut Enthalten in Loviscach, Jörn Deutsche Hydrografische Zeitschrift Springer Berlin Heidelberg, 2011 37(1984), 5 vom: Sept., Seite 173-200 1 Online-Ressource (21 MB, 00:25:44:00) (DE-627)1820839486 nnnm volume:37 year:1984 number:5 month:09 pages:173-200 https://dx.doi.org/10.1007/BF02226971 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER GBV_ILN_23 GBV_ILN_30 GBV_ILN_63 GBV_ILN_118 GBV_ILN_122 GBV_ILN_140 GBV_ILN_264 GBV_ILN_2057 GBV_ILN_2403 AR 37 1984 5 09 173-200 |
allfieldsSound |
10.1007/BF02226971 doi (DE-627)SPR055730604 (SPR)BF02226971-e DE-627 ger DE-627 rakwb eng Jankowski, Andrzej verfasserin aut Characteristics of horizontal macroturbulence due to the currents in the Baltic Sea 1984 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Deutsches Hydrographisches Institut 1984 Summary On the basis of current measurements in a number of sites in the southeastern and central Baltic, the following parameters of horizontal turbulence were estimated: components of turbulence intensity, moments of the correlation matrix, horizontal eddy-viscosity coefficients and directions of the extreme exchange in the horizontal plane. The exchange coefficients were calculated by the Ertel method. Exemplary empirical probability distribution (histograms) of the pulsations of current velocity components and the power spectra were shown. Changes in the turbulence parameters, depending upon the temporal scale the measure of which was assumed to be the averaging period of a cosine filter, were analysed. The influence of inertial oscillations upon the magnitudes of horizontal turbulence characteristics was shown. Power Spectrum (dpeaa)DE-He213 Current Velocity (dpeaa)DE-He213 Turbulence Intensity (dpeaa)DE-He213 Empirical Probability (dpeaa)DE-He213 Current Measurement (dpeaa)DE-He213 Catewicz, Zygmunt verfasserin aut Enthalten in Loviscach, Jörn Deutsche Hydrografische Zeitschrift Springer Berlin Heidelberg, 2011 37(1984), 5 vom: Sept., Seite 173-200 1 Online-Ressource (21 MB, 00:25:44:00) (DE-627)1820839486 nnnm volume:37 year:1984 number:5 month:09 pages:173-200 https://dx.doi.org/10.1007/BF02226971 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER GBV_ILN_23 GBV_ILN_30 GBV_ILN_63 GBV_ILN_118 GBV_ILN_122 GBV_ILN_140 GBV_ILN_264 GBV_ILN_2057 GBV_ILN_2403 AR 37 1984 5 09 173-200 |
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Characteristics of horizontal macroturbulence due to the currents in the Baltic Sea Power Spectrum (dpeaa)DE-He213 Current Velocity (dpeaa)DE-He213 Turbulence Intensity (dpeaa)DE-He213 Empirical Probability (dpeaa)DE-He213 Current Measurement (dpeaa)DE-He213 |
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Characteristics of horizontal macroturbulence due to the currents in the Baltic Sea |
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Summary On the basis of current measurements in a number of sites in the southeastern and central Baltic, the following parameters of horizontal turbulence were estimated: components of turbulence intensity, moments of the correlation matrix, horizontal eddy-viscosity coefficients and directions of the extreme exchange in the horizontal plane. The exchange coefficients were calculated by the Ertel method. Exemplary empirical probability distribution (histograms) of the pulsations of current velocity components and the power spectra were shown. Changes in the turbulence parameters, depending upon the temporal scale the measure of which was assumed to be the averaging period of a cosine filter, were analysed. The influence of inertial oscillations upon the magnitudes of horizontal turbulence characteristics was shown. © Deutsches Hydrographisches Institut 1984 |
abstractGer |
Summary On the basis of current measurements in a number of sites in the southeastern and central Baltic, the following parameters of horizontal turbulence were estimated: components of turbulence intensity, moments of the correlation matrix, horizontal eddy-viscosity coefficients and directions of the extreme exchange in the horizontal plane. The exchange coefficients were calculated by the Ertel method. Exemplary empirical probability distribution (histograms) of the pulsations of current velocity components and the power spectra were shown. Changes in the turbulence parameters, depending upon the temporal scale the measure of which was assumed to be the averaging period of a cosine filter, were analysed. The influence of inertial oscillations upon the magnitudes of horizontal turbulence characteristics was shown. © Deutsches Hydrographisches Institut 1984 |
abstract_unstemmed |
Summary On the basis of current measurements in a number of sites in the southeastern and central Baltic, the following parameters of horizontal turbulence were estimated: components of turbulence intensity, moments of the correlation matrix, horizontal eddy-viscosity coefficients and directions of the extreme exchange in the horizontal plane. The exchange coefficients were calculated by the Ertel method. Exemplary empirical probability distribution (histograms) of the pulsations of current velocity components and the power spectra were shown. Changes in the turbulence parameters, depending upon the temporal scale the measure of which was assumed to be the averaging period of a cosine filter, were analysed. The influence of inertial oscillations upon the magnitudes of horizontal turbulence characteristics was shown. © Deutsches Hydrographisches Institut 1984 |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">SPR055730604</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20240504064648.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">240504s1984 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF02226971</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR055730604</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)BF02226971-e</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="100" ind1="1" ind2=" "><subfield code="a">Jankowski, Andrzej</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Characteristics of horizontal macroturbulence due to the currents in the Baltic Sea</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1984</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">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Deutsches Hydrographisches Institut 1984</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Summary On the basis of current measurements in a number of sites in the southeastern and central Baltic, the following parameters of horizontal turbulence were estimated: components of turbulence intensity, moments of the correlation matrix, horizontal eddy-viscosity coefficients and directions of the extreme exchange in the horizontal plane. The exchange coefficients were calculated by the Ertel method. Exemplary empirical probability distribution (histograms) of the pulsations of current velocity components and the power spectra were shown. Changes in the turbulence parameters, depending upon the temporal scale the measure of which was assumed to be the averaging period of a cosine filter, were analysed. The influence of inertial oscillations upon the magnitudes of horizontal turbulence characteristics was shown.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Power Spectrum</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Current Velocity</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Turbulence Intensity</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Empirical Probability</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Current Measurement</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Catewicz, Zygmunt</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="a">Loviscach, Jörn</subfield><subfield code="t">Deutsche Hydrografische Zeitschrift</subfield><subfield code="d">Springer Berlin Heidelberg, 2011</subfield><subfield code="g">37(1984), 5 vom: Sept., Seite 173-200</subfield><subfield code="h">1 Online-Ressource (21 MB, 00:25:44:00)</subfield><subfield code="w">(DE-627)1820839486</subfield><subfield code="7">nnnm</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:37</subfield><subfield code="g">year:1984</subfield><subfield code="g">number:5</subfield><subfield code="g">month:09</subfield><subfield code="g">pages:173-200</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1007/BF02226971</subfield><subfield code="m">X:SPRINGER</subfield><subfield code="x">Resolving-System</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_0</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_SPRINGER</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_30</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_118</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_122</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_140</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_264</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2057</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2403</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">37</subfield><subfield code="j">1984</subfield><subfield code="e">5</subfield><subfield code="c">09</subfield><subfield code="h">173-200</subfield></datafield></record></collection>
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