The MJO skeleton model with observation‐based background state and forcing
The Madden–Julian Oscillation (MJO) skeleton model, a nonlinear oscillator model, has previously been shown to have solutions which exhibit several features in common with observed MJOs. In prior studies, model solutions have been found using mathematically simple (constant or sinusoidal) identical...
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Veröffentlicht in: | Quarterly journal of the Royal Meteorological Society 2015-10, Vol.141 (692), p.2654-2669 |
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description | The Madden–Julian Oscillation (MJO) skeleton model, a nonlinear oscillator model, has previously been shown to have solutions which exhibit several features in common with observed MJOs. In prior studies, model solutions have been found using mathematically simple (constant or sinusoidal) identical moistening and radiative forcing functions. Here we investigate whether this model can also produce realistic regional variability. To do this, observation‐based forcing functions are prescribed for latent heat flux and radiative cooling, and model solutions –both linear and nonlinear –are studied. In the stochastic nonlinear model, solutions reproduce the climatological mean convective activity well and the climatological variance reasonably well for such a simple model. In the linearized model, the solutions are found to contain additional structure including a realistic wave envelope of convective activity centred over the warm pool. These linear solutions are then used to identify and compare significant MJO activity in both reanalysis data and stochastic model solutions. Additional potential uses for these analytical and numerical solutions are discussed. |
doi_str_mv | 10.1002/qj.2552 |
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Reed ; Stechmann, Samuel N.</creator><creatorcontrib>Ogrosky, H. Reed ; Stechmann, Samuel N.</creatorcontrib><description>The Madden–Julian Oscillation (MJO) skeleton model, a nonlinear oscillator model, has previously been shown to have solutions which exhibit several features in common with observed MJOs. In prior studies, model solutions have been found using mathematically simple (constant or sinusoidal) identical moistening and radiative forcing functions. Here we investigate whether this model can also produce realistic regional variability. To do this, observation‐based forcing functions are prescribed for latent heat flux and radiative cooling, and model solutions –both linear and nonlinear –are studied. In the stochastic nonlinear model, solutions reproduce the climatological mean convective activity well and the climatological variance reasonably well for such a simple model. In the linearized model, the solutions are found to contain additional structure including a realistic wave envelope of convective activity centred over the warm pool. These linear solutions are then used to identify and compare significant MJO activity in both reanalysis data and stochastic model solutions. 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In the stochastic nonlinear model, solutions reproduce the climatological mean convective activity well and the climatological variance reasonably well for such a simple model. In the linearized model, the solutions are found to contain additional structure including a realistic wave envelope of convective activity centred over the warm pool. These linear solutions are then used to identify and compare significant MJO activity in both reanalysis data and stochastic model solutions. Additional potential uses for these analytical and numerical solutions are discussed.</description><subject>Cyclones</subject><subject>Latent heat</subject><subject>Madden–Julian Oscillation</subject><subject>Meteorology</subject><subject>MJO skeleton model</subject><subject>Stochastic models</subject><subject>tropical intraseasonal oscillation</subject><issn>0035-9009</issn><issn>1477-870X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2015</creationdate><recordtype>article</recordtype><recordid>eNp10M9Kw0AQBvBFFKxVfIUFDwqSOtlku8lRiv9KpQgVvIXdzWybNs22u4mlNx_BZ_RJTK0nQRiYOfz4GD5CzkPohQDsZj3vMc7ZAemEsRBBIuDtkHQAIh6kAOkxOfF-DgBcMNEho8kM6fNwTP0CS6xtRZc2x5JuinpGrfLo3mVd2Orr41NJjzlVUi-mzjZVTn0ta6SyvYx1uqimp-TIyNLj2e_uktf7u8ngMRiNH54Gt6NARyljgQZQJuGiHa1MP9YRTyFm0rA8RBRRzAFEIkyccKlYP4kgVUZhmjAUuZA86pKrfe7K2XWDvs6WhddYlrJC2_gsFG1iGMeQtPTiD53bxlXtd61ioh9xYDt1uVfaWe8dmmzliqV02yyEbNdqtp5nu1Zbeb2Xm6LE7X8sexn-6G_XSHbo</recordid><startdate>201510</startdate><enddate>201510</enddate><creator>Ogrosky, H. Reed</creator><creator>Stechmann, Samuel N.</creator><general>John Wiley & Sons, Ltd</general><general>Wiley Subscription Services, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>7UA</scope><scope>C1K</scope></search><sort><creationdate>201510</creationdate><title>The MJO skeleton model with observation‐based background state and forcing</title><author>Ogrosky, H. 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Reed</creatorcontrib><creatorcontrib>Stechmann, Samuel N.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><jtitle>Quarterly journal of the Royal Meteorological Society</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ogrosky, H. 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To do this, observation‐based forcing functions are prescribed for latent heat flux and radiative cooling, and model solutions –both linear and nonlinear –are studied. In the stochastic nonlinear model, solutions reproduce the climatological mean convective activity well and the climatological variance reasonably well for such a simple model. In the linearized model, the solutions are found to contain additional structure including a realistic wave envelope of convective activity centred over the warm pool. These linear solutions are then used to identify and compare significant MJO activity in both reanalysis data and stochastic model solutions. Additional potential uses for these analytical and numerical solutions are discussed.</abstract><cop>Chichester, UK</cop><pub>John Wiley & Sons, Ltd</pub><doi>10.1002/qj.2552</doi><tpages>16</tpages></addata></record> |
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subjects | Cyclones Latent heat Madden–Julian Oscillation Meteorology MJO skeleton model Stochastic models tropical intraseasonal oscillation |
title | The MJO skeleton model with observation‐based background state and forcing |
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