Tropical low formation and intensification over land as seen in ECMWF analyses
Case studies of the formation and intensification over land of three tropical lows in northern Australia are described. The case studies are based on European Centre for Medium‐Range Weather Forecasts (ECMWF) analyses. The aim is to investigate the generality of recent results concerning the dynamic...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Kilroy, Gerard [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2017 |
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| Rechteinformationen: |
Nutzungsrecht: © 2016 Royal Meteorological Society |
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| Schlagwörter: |
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| Systematik: |
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| Übergeordnetes Werk: |
Enthalten in: Quarterly journal of the Royal Meteorological Society - Reading : Soc., 1873, 143(2017), 703, Seite 772-784 |
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| Übergeordnetes Werk: |
volume:143 ; year:2017 ; number:703 ; pages:772-784 |
| Links: |
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| DOI / URN: |
10.1002/qj.2963 |
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OLC1991930836 |
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| 520 | |a Case studies of the formation and intensification over land of three tropical lows in northern Australia are described. The case studies are based on European Centre for Medium‐Range Weather Forecasts (ECMWF) analyses. The aim is to investigate the generality of recent results concerning the dynamics and thermodynamics of tropical lows. Consistent with these results, it is found that the processes of low formation and intensification are the same over land as over the ocean. An important element of the intensification process is the need for bursts of deep convection to persist near the circulation centre, which, in turn, requires that convective instability be maintained by surface moisture fluxes. The moist monsoonal environment locally surrounding the storm provides a shield against the adverse effects of dry‐air intrusion from the Australian continent. | ||
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tropical low formation and intensification over land as seen in ecmwf analyses |
| title_auth |
Tropical low formation and intensification over land as seen in ECMWF analyses |
| abstract |
Case studies of the formation and intensification over land of three tropical lows in northern Australia are described. The case studies are based on European Centre for Medium‐Range Weather Forecasts (ECMWF) analyses. The aim is to investigate the generality of recent results concerning the dynamics and thermodynamics of tropical lows. Consistent with these results, it is found that the processes of low formation and intensification are the same over land as over the ocean. An important element of the intensification process is the need for bursts of deep convection to persist near the circulation centre, which, in turn, requires that convective instability be maintained by surface moisture fluxes. The moist monsoonal environment locally surrounding the storm provides a shield against the adverse effects of dry‐air intrusion from the Australian continent. |
| abstractGer |
Case studies of the formation and intensification over land of three tropical lows in northern Australia are described. The case studies are based on European Centre for Medium‐Range Weather Forecasts (ECMWF) analyses. The aim is to investigate the generality of recent results concerning the dynamics and thermodynamics of tropical lows. Consistent with these results, it is found that the processes of low formation and intensification are the same over land as over the ocean. An important element of the intensification process is the need for bursts of deep convection to persist near the circulation centre, which, in turn, requires that convective instability be maintained by surface moisture fluxes. The moist monsoonal environment locally surrounding the storm provides a shield against the adverse effects of dry‐air intrusion from the Australian continent. |
| abstract_unstemmed |
Case studies of the formation and intensification over land of three tropical lows in northern Australia are described. The case studies are based on European Centre for Medium‐Range Weather Forecasts (ECMWF) analyses. The aim is to investigate the generality of recent results concerning the dynamics and thermodynamics of tropical lows. Consistent with these results, it is found that the processes of low formation and intensification are the same over land as over the ocean. An important element of the intensification process is the need for bursts of deep convection to persist near the circulation centre, which, in turn, requires that convective instability be maintained by surface moisture fluxes. The moist monsoonal environment locally surrounding the storm provides a shield against the adverse effects of dry‐air intrusion from the Australian continent. |
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| title_short |
Tropical low formation and intensification over land as seen in ECMWF analyses |
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http://dx.doi.org/10.1002/qj.2963 http://onlinelibrary.wiley.com/doi/10.1002/qj.2963/abstract http://search.proquest.com/docview/1884064394 |
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