Changes
On March 6, 2023 at 5:03:02 PM UTC,
-
Added field
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with valuehttps://www.dora.lib4ri.ch/eawag/islandora/object/eawag:30177
to Data for: Penetrative Convection Modifies the Dynamics of Downslope Gravity Currents
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2 | "author": "[\"Doda, Tomy\", \"Ulloa, Hugo. N.\", \"Ram\\u00f3n, | 2 | "author": "[\"Doda, Tomy\", \"Ulloa, Hugo. N.\", \"Ram\\u00f3n, | ||
3 | Cintia L.\", \"W\\u00fcest, Alfred\", \"Bouffard, Damien\"]", | 3 | Cintia L.\", \"W\\u00fcest, Alfred\", \"Bouffard, Damien\"]", | ||
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10 | A., & Bouffard, D. (2022). Data for: Penetrative Convection | 10 | A., & Bouffard, D. (2022). Data for: Penetrative Convection | ||
11 | Modifies the Dynamics of Downslope Gravity Currents (Version 1.0). | 11 | Modifies the Dynamics of Downslope Gravity Currents (Version 1.0). | ||
12 | Eawag: Swiss Federal Institute of Aquatic Science and Technology. | 12 | Eawag: Swiss Federal Institute of Aquatic Science and Technology. | ||
13 | https://doi.org/10.25678/0007PR" | 13 | https://doi.org/10.25678/0007PR" | ||
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18 | A., & Bouffard, D. (2023). Penetrative Convection Modifies the | 18 | A., & Bouffard, D. (2023). Penetrative Convection Modifies the | ||
19 | Dynamics of Downslope Gravity Currents. Geophysical Research Letters, | 19 | Dynamics of Downslope Gravity Currents. Geophysical Research Letters, | ||
20 | 50(2). https://doi.org/10.1029/2022gl100633\n" | 20 | 50(2). https://doi.org/10.1029/2022gl100633\n" | ||
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106 | "maintainer": "Doda, Tomy", | 111 | "maintainer": "Doda, Tomy", | ||
107 | "maintainer_email": "Bouffard, Damien <Damien.Bouffard@eawag.ch>", | 112 | "maintainer_email": "Bouffard, Damien <Damien.Bouffard@eawag.ch>", | ||
108 | "metadata_created": "2023-01-30T14:42:48.061296", | 113 | "metadata_created": "2023-01-30T14:42:48.061296", | ||
109 | "metadata_modified": "2023-01-30T14:42:48.061306", | 114 | "metadata_modified": "2023-01-30T14:42:48.061306", | ||
110 | "name": | 115 | "name": | ||
111 | ative-convection-modifies-the-dynamics-of-downslope-gravity-currents", | 116 | ative-convection-modifies-the-dynamics-of-downslope-gravity-currents", | ||
112 | "notes": "Gravity currents contribute to the transport of heat and | 117 | "notes": "Gravity currents contribute to the transport of heat and | ||
113 | mass in atmospheric and aquatic environments. In aquatic systems | 118 | mass in atmospheric and aquatic environments. In aquatic systems | ||
114 | subject to daily surface cooling, gravity currents propagate through | 119 | subject to daily surface cooling, gravity currents propagate through | ||
115 | turbulent convective surroundings. Yet, the effects of thermal | 120 | turbulent convective surroundings. Yet, the effects of thermal | ||
116 | convection on aquatic gravity currents remain to be quantified. This | 121 | convection on aquatic gravity currents remain to be quantified. This | ||
117 | paper demonstrates how the interaction between penetrative convection | 122 | paper demonstrates how the interaction between penetrative convection | ||
118 | and downslope gravity currents impacts the fluid dynamics and | 123 | and downslope gravity currents impacts the fluid dynamics and | ||
119 | transport across littoral aquatic systems. We performed field | 124 | transport across littoral aquatic systems. We performed field | ||
120 | experiments in a wind-sheltered lake experiencing differential cooling | 125 | experiments in a wind-sheltered lake experiencing differential cooling | ||
121 | to resolve the dynamics of thermally driven gravity currents in | 126 | to resolve the dynamics of thermally driven gravity currents in | ||
122 | convective environments. Our in situ observations reveal that | 127 | convective environments. Our in situ observations reveal that | ||
123 | convective plumes penetrate gravity currents, generating large | 128 | convective plumes penetrate gravity currents, generating large | ||
124 | vertical fluctuations that foster the erosion of the stratified layer. | 129 | vertical fluctuations that foster the erosion of the stratified layer. | ||
125 | This enhanced vertical mixing destroys the stratified downslope flow | 130 | This enhanced vertical mixing destroys the stratified downslope flow | ||
126 | and limits the basin-scale transport. Our results demonstrate that the | 131 | and limits the basin-scale transport. Our results demonstrate that the | ||
127 | interaction between penetrative convection and downslope gravity | 132 | interaction between penetrative convection and downslope gravity | ||
128 | currents controls the littoral-pelagic connectivity in aquatic | 133 | currents controls the littoral-pelagic connectivity in aquatic | ||
129 | ecosystems.", | 134 | ecosystems.", | ||
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135 | "description": "The Aquatic Physics Group studies physical | 140 | "description": "The Aquatic Physics Group studies physical | ||
136 | processes mainly in lakes, reservoirs and rivers. We have two | 141 | processes mainly in lakes, reservoirs and rivers. We have two | ||
137 | approaches:\r\n\r\n+ From small scale in situ turbulence measurements | 142 | approaches:\r\n\r\n+ From small scale in situ turbulence measurements | ||
138 | to large scale three-dimensional models.\r\n\r\n+ Aquatic physics as a | 143 | to large scale three-dimensional models.\r\n\r\n+ Aquatic physics as a | ||
139 | tool to understand aquatic systems.\r\n\r\nOur research consists in | 144 | tool to understand aquatic systems.\r\n\r\nOur research consists in | ||
140 | dedicated in-situ measurements together with large scale three | 145 | dedicated in-situ measurements together with large scale three | ||
141 | dimensional numerical models. This approach is perfectly fitted to | 146 | dimensional numerical models. This approach is perfectly fitted to | ||
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332 | Downslope Gravity Currents", | 337 | Downslope Gravity Currents", | ||
333 | "type": "dataset", | 338 | "type": "dataset", | ||
334 | "url": "https://doi.org/10.25678/0007PR/", | 339 | "url": "https://doi.org/10.25678/0007PR/", | ||
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336 | } | 341 | } |