Determining the Velocity of the Upper Layer of Lake Ladoga by Means of Maximum Cross Correlation (MCC)
The first use of Maximum Cross Correlation to calculate the surface currents of Lake Ladoga yields very promising results in the absence of direct measurements of currents. The technique is adapted for a large lake, and new procedures are proposed for selecting the most informative infrared satellit...
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| Veröffentlicht in: | Izvestiya. Atmospheric and oceanic physics 2020-12, Vol.56 (12), p.1678-1686 |
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| container_title | Izvestiya. Atmospheric and oceanic physics |
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| creator | Guzivaty, V. V. Naumenko, M. A. Rumyantsev, V. A. |
| description | The first use of Maximum Cross Correlation to calculate the surface currents of Lake Ladoga yields very promising results in the absence of direct measurements of currents. The technique is adapted for a large lake, and new procedures are proposed for selecting the most informative infrared satellite surveys for lake flow analysis. The best conditions, parameters, and limitations of using Maximum Cross Correlation for Lake Ladoga are obtained. Surface current systems are constructed for specific wind situations in the open water period. The technique, based on an analysis of successive satellite IR surveys of Lake Ladoga’s surface, allows the dynamics of the waters to be determined and can be applied to other large lakes. |
| doi_str_mv | 10.1134/S0001433820120415 |
| format | Article |
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The technique, based on an analysis of successive satellite IR surveys of Lake Ladoga’s surface, allows the dynamics of the waters to be determined and can be applied to other large lakes.</description><subject>Climatology</subject><subject>Correlation</subject><subject>Cross correlation</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geophysics/Geodesy</subject><subject>Infrared analysis</subject><subject>Lakes</subject><subject>Polls & surveys</subject><subject>Satellites</subject><subject>Surface currents</subject><subject>Surveys</subject><subject>Ways and Means of Processing and Interpreting Space-Based Information</subject><issn>0001-4338</issn><issn>1555-628X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp1UDtPwzAQthBIlMIPYLPEAkPAvtixM6JQHlIqBihii-zUKSlNHOxUIv8ehyIxIJY73X2PeyB0SsklpTG7eiKEUBbHEggFwijfQxPKOY8SkK_7aDLC0YgfoiPv14QkwIiYoOrG9MY1dVu3K9y_GfxiNras-wHb6rtedJ1xOFdDiKGVq3cTwtKuFNYDnhvV-rE_V591s21w5qz3OLPOmY3qa9vi83mWXRyjg0ptvDn5yVO0uJ09Z_dR_nj3kF3nUQmJ7KNSaQNaVABloiSRUsNSSJlCmpiUioCE-ypFypgJTmMhJPAUNNdLDZAIFU_R2c63c_Zja3xfrO3WtWFkASxNGWFSpIFFd6xy3NaZquhc3Sg3FJQU4zuLP-8MGthpfOC2K-N-nf8XfQH1uXSA</recordid><startdate>20201201</startdate><enddate>20201201</enddate><creator>Guzivaty, V. 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| ispartof | Izvestiya. Atmospheric and oceanic physics, 2020-12, Vol.56 (12), p.1678-1686 |
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| subjects | Climatology Correlation Cross correlation Earth and Environmental Science Earth Sciences Geophysics/Geodesy Infrared analysis Lakes Polls & surveys Satellites Surface currents Surveys Ways and Means of Processing and Interpreting Space-Based Information |
| title | Determining the Velocity of the Upper Layer of Lake Ladoga by Means of Maximum Cross Correlation (MCC) |
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