Analysis and modeling of a tropical-like cyclonein the Mediterranean Sea
Summary The storm formed over the warm waters between Sicily and Libya in a region of weak flow ahead of a cold, upper-level trough. During its 5-day lifetime it moved erratically before dissipating off the Turkish coast. As the storm developed, it diminished in size, assuming a hurricane-like appea...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Reed, R. J. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2001 |
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| Schlagwörter: |
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| Systematik: |
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| Anmerkung: |
© Springer-Verlag Wien 2001 |
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| Übergeordnetes Werk: |
Enthalten in: Meteorology and atmospheric physics - Springer-Verlag, 1986, 76(2001), 3 vom: Apr., Seite 183-202 |
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| Übergeordnetes Werk: |
volume:76 ; year:2001 ; number:3 ; month:04 ; pages:183-202 |
| Links: |
|---|
| DOI / URN: |
10.1007/s007030170029 |
|---|
| Katalog-ID: |
OLC2030081701 |
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| 520 | |a Summary The storm formed over the warm waters between Sicily and Libya in a region of weak flow ahead of a cold, upper-level trough. During its 5-day lifetime it moved erratically before dissipating off the Turkish coast. As the storm developed, it diminished in size, assuming a hurricane-like appearance in satellite imagery. Ships near the vortex center reported near-hurricane force winds. An attempt to simulate the storm development with a state-of-the-art mesoscale model met with mixed success. The most serious errors occurred after the initial deepening when the predicted track departed substantially from the observed and the contraction of the storm to mesoscale dimension was missed. A number of forward and adjoint sensitivity experiments were conducted to identify factors influencing the development and to explore ways of improving the prediction. The most realistic prediction was achieved by implanting a vortex, in the manner commonly done in tropical cyclone prediction, at an early stage in the storm’s history and by using, in addition, adjoint sensitivity to further modify the initial conditions. | ||
| 650 | 4 | |a Vortex | |
| 650 | 4 | |a Cyclone | |
| 650 | 4 | |a Tropical Cyclone | |
| 650 | 4 | |a Warm Water | |
| 650 | 4 | |a Satellite Imagery | |
| 700 | 1 | |a Kuo, Y.-H. |4 aut | |
| 700 | 1 | |a Albright, M. D. |4 aut | |
| 700 | 1 | |a Gao, K. |4 aut | |
| 700 | 1 | |a Guo, Y.-R. |4 aut | |
| 700 | 1 | |a Huang, W. |4 aut | |
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10.1007/s007030170029 doi (DE-627)OLC2030081701 (DE-He213)s007030170029-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn RA 1000 VZ rvk Reed, R. J. verfasserin aut Analysis and modeling of a tropical-like cyclonein the Mediterranean Sea 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2001 Summary The storm formed over the warm waters between Sicily and Libya in a region of weak flow ahead of a cold, upper-level trough. During its 5-day lifetime it moved erratically before dissipating off the Turkish coast. As the storm developed, it diminished in size, assuming a hurricane-like appearance in satellite imagery. Ships near the vortex center reported near-hurricane force winds. An attempt to simulate the storm development with a state-of-the-art mesoscale model met with mixed success. The most serious errors occurred after the initial deepening when the predicted track departed substantially from the observed and the contraction of the storm to mesoscale dimension was missed. A number of forward and adjoint sensitivity experiments were conducted to identify factors influencing the development and to explore ways of improving the prediction. The most realistic prediction was achieved by implanting a vortex, in the manner commonly done in tropical cyclone prediction, at an early stage in the storm’s history and by using, in addition, adjoint sensitivity to further modify the initial conditions. Vortex Cyclone Tropical Cyclone Warm Water Satellite Imagery Kuo, Y.-H. aut Albright, M. D. aut Gao, K. aut Guo, Y.-R. aut Huang, W. aut Enthalten in Meteorology and atmospheric physics Springer-Verlag, 1986 76(2001), 3 vom: Apr., Seite 183-202 (DE-627)129582492 (DE-600)232907-4 (DE-576)015076032 0177-7971 nnns volume:76 year:2001 number:3 month:04 pages:183-202 https://doi.org/10.1007/s007030170029 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2001 GBV_ILN_2006 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4029 RA 1000 AR 76 2001 3 04 183-202 |
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10.1007/s007030170029 doi (DE-627)OLC2030081701 (DE-He213)s007030170029-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn RA 1000 VZ rvk Reed, R. J. verfasserin aut Analysis and modeling of a tropical-like cyclonein the Mediterranean Sea 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2001 Summary The storm formed over the warm waters between Sicily and Libya in a region of weak flow ahead of a cold, upper-level trough. During its 5-day lifetime it moved erratically before dissipating off the Turkish coast. As the storm developed, it diminished in size, assuming a hurricane-like appearance in satellite imagery. Ships near the vortex center reported near-hurricane force winds. An attempt to simulate the storm development with a state-of-the-art mesoscale model met with mixed success. The most serious errors occurred after the initial deepening when the predicted track departed substantially from the observed and the contraction of the storm to mesoscale dimension was missed. A number of forward and adjoint sensitivity experiments were conducted to identify factors influencing the development and to explore ways of improving the prediction. The most realistic prediction was achieved by implanting a vortex, in the manner commonly done in tropical cyclone prediction, at an early stage in the storm’s history and by using, in addition, adjoint sensitivity to further modify the initial conditions. Vortex Cyclone Tropical Cyclone Warm Water Satellite Imagery Kuo, Y.-H. aut Albright, M. D. aut Gao, K. aut Guo, Y.-R. aut Huang, W. aut Enthalten in Meteorology and atmospheric physics Springer-Verlag, 1986 76(2001), 3 vom: Apr., Seite 183-202 (DE-627)129582492 (DE-600)232907-4 (DE-576)015076032 0177-7971 nnns volume:76 year:2001 number:3 month:04 pages:183-202 https://doi.org/10.1007/s007030170029 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2001 GBV_ILN_2006 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4029 RA 1000 AR 76 2001 3 04 183-202 |
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10.1007/s007030170029 doi (DE-627)OLC2030081701 (DE-He213)s007030170029-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn RA 1000 VZ rvk Reed, R. J. verfasserin aut Analysis and modeling of a tropical-like cyclonein the Mediterranean Sea 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2001 Summary The storm formed over the warm waters between Sicily and Libya in a region of weak flow ahead of a cold, upper-level trough. During its 5-day lifetime it moved erratically before dissipating off the Turkish coast. As the storm developed, it diminished in size, assuming a hurricane-like appearance in satellite imagery. Ships near the vortex center reported near-hurricane force winds. An attempt to simulate the storm development with a state-of-the-art mesoscale model met with mixed success. The most serious errors occurred after the initial deepening when the predicted track departed substantially from the observed and the contraction of the storm to mesoscale dimension was missed. A number of forward and adjoint sensitivity experiments were conducted to identify factors influencing the development and to explore ways of improving the prediction. The most realistic prediction was achieved by implanting a vortex, in the manner commonly done in tropical cyclone prediction, at an early stage in the storm’s history and by using, in addition, adjoint sensitivity to further modify the initial conditions. Vortex Cyclone Tropical Cyclone Warm Water Satellite Imagery Kuo, Y.-H. aut Albright, M. D. aut Gao, K. aut Guo, Y.-R. aut Huang, W. aut Enthalten in Meteorology and atmospheric physics Springer-Verlag, 1986 76(2001), 3 vom: Apr., Seite 183-202 (DE-627)129582492 (DE-600)232907-4 (DE-576)015076032 0177-7971 nnns volume:76 year:2001 number:3 month:04 pages:183-202 https://doi.org/10.1007/s007030170029 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2001 GBV_ILN_2006 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4029 RA 1000 AR 76 2001 3 04 183-202 |
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10.1007/s007030170029 doi (DE-627)OLC2030081701 (DE-He213)s007030170029-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn RA 1000 VZ rvk Reed, R. J. verfasserin aut Analysis and modeling of a tropical-like cyclonein the Mediterranean Sea 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2001 Summary The storm formed over the warm waters between Sicily and Libya in a region of weak flow ahead of a cold, upper-level trough. During its 5-day lifetime it moved erratically before dissipating off the Turkish coast. As the storm developed, it diminished in size, assuming a hurricane-like appearance in satellite imagery. Ships near the vortex center reported near-hurricane force winds. An attempt to simulate the storm development with a state-of-the-art mesoscale model met with mixed success. The most serious errors occurred after the initial deepening when the predicted track departed substantially from the observed and the contraction of the storm to mesoscale dimension was missed. A number of forward and adjoint sensitivity experiments were conducted to identify factors influencing the development and to explore ways of improving the prediction. The most realistic prediction was achieved by implanting a vortex, in the manner commonly done in tropical cyclone prediction, at an early stage in the storm’s history and by using, in addition, adjoint sensitivity to further modify the initial conditions. Vortex Cyclone Tropical Cyclone Warm Water Satellite Imagery Kuo, Y.-H. aut Albright, M. D. aut Gao, K. aut Guo, Y.-R. aut Huang, W. aut Enthalten in Meteorology and atmospheric physics Springer-Verlag, 1986 76(2001), 3 vom: Apr., Seite 183-202 (DE-627)129582492 (DE-600)232907-4 (DE-576)015076032 0177-7971 nnns volume:76 year:2001 number:3 month:04 pages:183-202 https://doi.org/10.1007/s007030170029 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2001 GBV_ILN_2006 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4029 RA 1000 AR 76 2001 3 04 183-202 |
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10.1007/s007030170029 doi (DE-627)OLC2030081701 (DE-He213)s007030170029-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn RA 1000 VZ rvk Reed, R. J. verfasserin aut Analysis and modeling of a tropical-like cyclonein the Mediterranean Sea 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2001 Summary The storm formed over the warm waters between Sicily and Libya in a region of weak flow ahead of a cold, upper-level trough. During its 5-day lifetime it moved erratically before dissipating off the Turkish coast. As the storm developed, it diminished in size, assuming a hurricane-like appearance in satellite imagery. Ships near the vortex center reported near-hurricane force winds. An attempt to simulate the storm development with a state-of-the-art mesoscale model met with mixed success. The most serious errors occurred after the initial deepening when the predicted track departed substantially from the observed and the contraction of the storm to mesoscale dimension was missed. A number of forward and adjoint sensitivity experiments were conducted to identify factors influencing the development and to explore ways of improving the prediction. The most realistic prediction was achieved by implanting a vortex, in the manner commonly done in tropical cyclone prediction, at an early stage in the storm’s history and by using, in addition, adjoint sensitivity to further modify the initial conditions. Vortex Cyclone Tropical Cyclone Warm Water Satellite Imagery Kuo, Y.-H. aut Albright, M. D. aut Gao, K. aut Guo, Y.-R. aut Huang, W. aut Enthalten in Meteorology and atmospheric physics Springer-Verlag, 1986 76(2001), 3 vom: Apr., Seite 183-202 (DE-627)129582492 (DE-600)232907-4 (DE-576)015076032 0177-7971 nnns volume:76 year:2001 number:3 month:04 pages:183-202 https://doi.org/10.1007/s007030170029 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2001 GBV_ILN_2006 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4029 RA 1000 AR 76 2001 3 04 183-202 |
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Analysis and modeling of a tropical-like cyclonein the Mediterranean Sea |
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Analysis and modeling of a tropical-like cyclonein the Mediterranean Sea |
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Reed, R. J. |
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Meteorology and atmospheric physics |
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2001 |
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Reed, R. J. Kuo, Y.-H. Albright, M. D. Gao, K. Guo, Y.-R. Huang, W. |
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76 |
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Reed, R. J. |
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10.1007/s007030170029 |
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550 |
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analysis and modeling of a tropical-like cyclonein the mediterranean sea |
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Analysis and modeling of a tropical-like cyclonein the Mediterranean Sea |
| abstract |
Summary The storm formed over the warm waters between Sicily and Libya in a region of weak flow ahead of a cold, upper-level trough. During its 5-day lifetime it moved erratically before dissipating off the Turkish coast. As the storm developed, it diminished in size, assuming a hurricane-like appearance in satellite imagery. Ships near the vortex center reported near-hurricane force winds. An attempt to simulate the storm development with a state-of-the-art mesoscale model met with mixed success. The most serious errors occurred after the initial deepening when the predicted track departed substantially from the observed and the contraction of the storm to mesoscale dimension was missed. A number of forward and adjoint sensitivity experiments were conducted to identify factors influencing the development and to explore ways of improving the prediction. The most realistic prediction was achieved by implanting a vortex, in the manner commonly done in tropical cyclone prediction, at an early stage in the storm’s history and by using, in addition, adjoint sensitivity to further modify the initial conditions. © Springer-Verlag Wien 2001 |
| abstractGer |
Summary The storm formed over the warm waters between Sicily and Libya in a region of weak flow ahead of a cold, upper-level trough. During its 5-day lifetime it moved erratically before dissipating off the Turkish coast. As the storm developed, it diminished in size, assuming a hurricane-like appearance in satellite imagery. Ships near the vortex center reported near-hurricane force winds. An attempt to simulate the storm development with a state-of-the-art mesoscale model met with mixed success. The most serious errors occurred after the initial deepening when the predicted track departed substantially from the observed and the contraction of the storm to mesoscale dimension was missed. A number of forward and adjoint sensitivity experiments were conducted to identify factors influencing the development and to explore ways of improving the prediction. The most realistic prediction was achieved by implanting a vortex, in the manner commonly done in tropical cyclone prediction, at an early stage in the storm’s history and by using, in addition, adjoint sensitivity to further modify the initial conditions. © Springer-Verlag Wien 2001 |
| abstract_unstemmed |
Summary The storm formed over the warm waters between Sicily and Libya in a region of weak flow ahead of a cold, upper-level trough. During its 5-day lifetime it moved erratically before dissipating off the Turkish coast. As the storm developed, it diminished in size, assuming a hurricane-like appearance in satellite imagery. Ships near the vortex center reported near-hurricane force winds. An attempt to simulate the storm development with a state-of-the-art mesoscale model met with mixed success. The most serious errors occurred after the initial deepening when the predicted track departed substantially from the observed and the contraction of the storm to mesoscale dimension was missed. A number of forward and adjoint sensitivity experiments were conducted to identify factors influencing the development and to explore ways of improving the prediction. The most realistic prediction was achieved by implanting a vortex, in the manner commonly done in tropical cyclone prediction, at an early stage in the storm’s history and by using, in addition, adjoint sensitivity to further modify the initial conditions. © Springer-Verlag Wien 2001 |
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Analysis and modeling of a tropical-like cyclonein the Mediterranean Sea |
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