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Horizontal Pressure Gradient Parameterization for One‐Dimensional Lake Models
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| Zeitschriftentitel: | Journal of Advances in Modeling Earth Systems |
|---|---|
| Personen und Körperschaften: | , , |
| In: | Journal of Advances in Modeling Earth Systems, 12, 2020, 2 |
| Format: | E-Article |
| Sprache: | Englisch |
| veröffentlicht: |
American Geophysical Union (AGU)
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| Schlagwörter: |
| author_facet |
Stepanenko, V. M. Valerio, G. Pilotti, M. Stepanenko, V. M. Valerio, G. Pilotti, M. |
|---|---|
| author |
Stepanenko, V. M. Valerio, G. Pilotti, M. |
| spellingShingle |
Stepanenko, V. M. Valerio, G. Pilotti, M. Journal of Advances in Modeling Earth Systems Horizontal Pressure Gradient Parameterization for One‐Dimensional Lake Models General Earth and Planetary Sciences Environmental Chemistry Global and Planetary Change |
| author_sort |
stepanenko, v. m. |
| spelling |
Stepanenko, V. M. Valerio, G. Pilotti, M. 1942-2466 1942-2466 American Geophysical Union (AGU) General Earth and Planetary Sciences Environmental Chemistry Global and Planetary Change http://dx.doi.org/10.1029/2019ms001906 <jats:title>Abstract</jats:title><jats:p>This work presents a new method for closure of horizontally averaged 1‐D thermohydrodynamic equations in an enclosed reservoir by parameterizing the horizontal pressure gradient usually omitted in 1‐D lake models. Horizontal pressure gradient is computed using an auxiliary multilayer model where horizontal structure of speed and pressure is given by 1‐st Fourier mode. A major effect of new parameterization in 1‐D lake model is the emergence of explicitly reproduced H1 seiche modes. The parameterization is implemented in the LAKE model, with minor (2–4%) extra computational cost imposed. The model is applied to Lake Iseo (Italy), and calculated temperature series are compared to measured ones in upper, middle, and deep portions of metalimnion. The amplitude of seiche‐induced temperature oscillations well matched the observed amplitude by tuning the bottom friction coefficient only. The synoptic variability of thermocline vertical displacement caused by wind events is well reproduced by the model. The dominant peak of quasi‐diurnal period in temperature power spectrum was captured in simulations as well. Using the new parameterization of horizontal pressure gradient extends the applicability of a 1‐D lake model formulation to small lakes, which size is less than internal Rossby radius, and where pressure gradient dominates over Coriolis force.</jats:p> Horizontal Pressure Gradient Parameterization for One‐Dimensional Lake Models Journal of Advances in Modeling Earth Systems |
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10.1029/2019ms001906 |
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American Geophysical Union (AGU), 2020 |
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Journal of Advances in Modeling Earth Systems |
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| title |
Horizontal Pressure Gradient Parameterization for One‐Dimensional Lake Models |
| title_unstemmed |
Horizontal Pressure Gradient Parameterization for One‐Dimensional Lake Models |
| title_full |
Horizontal Pressure Gradient Parameterization for One‐Dimensional Lake Models |
| title_fullStr |
Horizontal Pressure Gradient Parameterization for One‐Dimensional Lake Models |
| title_full_unstemmed |
Horizontal Pressure Gradient Parameterization for One‐Dimensional Lake Models |
| title_short |
Horizontal Pressure Gradient Parameterization for One‐Dimensional Lake Models |
| title_sort |
horizontal pressure gradient parameterization for one‐dimensional lake models |
| topic |
General Earth and Planetary Sciences Environmental Chemistry Global and Planetary Change |
| url |
http://dx.doi.org/10.1029/2019ms001906 |
| publishDate |
2020 |
| physical |
|
| description |
<jats:title>Abstract</jats:title><jats:p>This work presents a new method for closure of horizontally averaged 1‐D thermohydrodynamic equations in an enclosed reservoir by parameterizing the horizontal pressure gradient usually omitted in 1‐D lake models. Horizontal pressure gradient is computed using an auxiliary multilayer model where horizontal structure of speed and pressure is given by 1‐st Fourier mode. A major effect of new parameterization in 1‐D lake model is the emergence of explicitly reproduced H1 seiche modes. The parameterization is implemented in the LAKE model, with minor (2–4%) extra computational cost imposed. The model is applied to Lake Iseo (Italy), and calculated temperature series are compared to measured ones in upper, middle, and deep portions of metalimnion. The amplitude of seiche‐induced temperature oscillations well matched the observed amplitude by tuning the bottom friction coefficient only. The synoptic variability of thermocline vertical displacement caused by wind events is well reproduced by the model. The dominant peak of quasi‐diurnal period in temperature power spectrum was captured in simulations as well. Using the new parameterization of horizontal pressure gradient extends the applicability of a 1‐D lake model formulation to small lakes, which size is less than internal Rossby radius, and where pressure gradient dominates over Coriolis force.</jats:p> |
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| author | Stepanenko, V. M., Valerio, G., Pilotti, M. |
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| description | <jats:title>Abstract</jats:title><jats:p>This work presents a new method for closure of horizontally averaged 1‐D thermohydrodynamic equations in an enclosed reservoir by parameterizing the horizontal pressure gradient usually omitted in 1‐D lake models. Horizontal pressure gradient is computed using an auxiliary multilayer model where horizontal structure of speed and pressure is given by 1‐st Fourier mode. A major effect of new parameterization in 1‐D lake model is the emergence of explicitly reproduced H1 seiche modes. The parameterization is implemented in the LAKE model, with minor (2–4%) extra computational cost imposed. The model is applied to Lake Iseo (Italy), and calculated temperature series are compared to measured ones in upper, middle, and deep portions of metalimnion. The amplitude of seiche‐induced temperature oscillations well matched the observed amplitude by tuning the bottom friction coefficient only. The synoptic variability of thermocline vertical displacement caused by wind events is well reproduced by the model. The dominant peak of quasi‐diurnal period in temperature power spectrum was captured in simulations as well. Using the new parameterization of horizontal pressure gradient extends the applicability of a 1‐D lake model formulation to small lakes, which size is less than internal Rossby radius, and where pressure gradient dominates over Coriolis force.</jats:p> |
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| spelling | Stepanenko, V. M. Valerio, G. Pilotti, M. 1942-2466 1942-2466 American Geophysical Union (AGU) General Earth and Planetary Sciences Environmental Chemistry Global and Planetary Change http://dx.doi.org/10.1029/2019ms001906 <jats:title>Abstract</jats:title><jats:p>This work presents a new method for closure of horizontally averaged 1‐D thermohydrodynamic equations in an enclosed reservoir by parameterizing the horizontal pressure gradient usually omitted in 1‐D lake models. Horizontal pressure gradient is computed using an auxiliary multilayer model where horizontal structure of speed and pressure is given by 1‐st Fourier mode. A major effect of new parameterization in 1‐D lake model is the emergence of explicitly reproduced H1 seiche modes. The parameterization is implemented in the LAKE model, with minor (2–4%) extra computational cost imposed. The model is applied to Lake Iseo (Italy), and calculated temperature series are compared to measured ones in upper, middle, and deep portions of metalimnion. The amplitude of seiche‐induced temperature oscillations well matched the observed amplitude by tuning the bottom friction coefficient only. The synoptic variability of thermocline vertical displacement caused by wind events is well reproduced by the model. The dominant peak of quasi‐diurnal period in temperature power spectrum was captured in simulations as well. Using the new parameterization of horizontal pressure gradient extends the applicability of a 1‐D lake model formulation to small lakes, which size is less than internal Rossby radius, and where pressure gradient dominates over Coriolis force.</jats:p> Horizontal Pressure Gradient Parameterization for One‐Dimensional Lake Models Journal of Advances in Modeling Earth Systems |
| spellingShingle | Stepanenko, V. M., Valerio, G., Pilotti, M., Journal of Advances in Modeling Earth Systems, Horizontal Pressure Gradient Parameterization for One‐Dimensional Lake Models, General Earth and Planetary Sciences, Environmental Chemistry, Global and Planetary Change |
| title | Horizontal Pressure Gradient Parameterization for One‐Dimensional Lake Models |
| title_full | Horizontal Pressure Gradient Parameterization for One‐Dimensional Lake Models |
| title_fullStr | Horizontal Pressure Gradient Parameterization for One‐Dimensional Lake Models |
| title_full_unstemmed | Horizontal Pressure Gradient Parameterization for One‐Dimensional Lake Models |
| title_short | Horizontal Pressure Gradient Parameterization for One‐Dimensional Lake Models |
| title_sort | horizontal pressure gradient parameterization for one‐dimensional lake models |
| title_unstemmed | Horizontal Pressure Gradient Parameterization for One‐Dimensional Lake Models |
| topic | General Earth and Planetary Sciences, Environmental Chemistry, Global and Planetary Change |
| url | http://dx.doi.org/10.1029/2019ms001906 |