Construction of synthetic ocean wave series along the Colombian Caribbean Coast: A wave climate analysis
• A methodology was applied to generate synthetic waves series (mean and extreme). • Seasonal variability is generally controlled by trade winds and the hurricane events. • A dipole between the north-east (hurricanes) and the south-west (cold fronts) is found. • During DJF and MAM seasons, in El Niñ...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Osorio, Andrés F. [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2016 |
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| Schlagwörter: |
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| Umfang: |
13 |
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| Übergeordnetes Werk: |
Enthalten in: P-602 - The attitudes of students of high schools in Gjilan related to drug abuse - 2012, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:56 ; year:2016 ; pages:119-131 ; extent:13 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.apor.2016.01.004 |
|---|
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ELV029459966 |
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| 520 | |a • A methodology was applied to generate synthetic waves series (mean and extreme). • Seasonal variability is generally controlled by trade winds and the hurricane events. • A dipole between the north-east (hurricanes) and the south-west (cold fronts) is found. • During DJF and MAM seasons, in El Niño years low values of wave height occur. • During the JJA season, the highest values occurring during El Niño. | ||
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10.1016/j.apor.2016.01.004 doi GBVA2016002000016.pica (DE-627)ELV029459966 (ELSEVIER)S0141-1187(16)30002-5 DE-627 ger DE-627 rakwb eng 550 570 550 DE-600 570 DE-600 610 VZ 530 VZ 33.00 bkl Osorio, Andrés F. verfasserin aut Construction of synthetic ocean wave series along the Colombian Caribbean Coast: A wave climate analysis 2016 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • A methodology was applied to generate synthetic waves series (mean and extreme). • Seasonal variability is generally controlled by trade winds and the hurricane events. • A dipole between the north-east (hurricanes) and the south-west (cold fronts) is found. • During DJF and MAM seasons, in El Niño years low values of wave height occur. • During the JJA season, the highest values occurring during El Niño. Colombia Elsevier Synthetic series Elsevier Caribbean Sea Elsevier Waves Elsevier Hurricane waves Elsevier Montoya, Rubén D. oth Ortiz, Juan Carlos oth Peláez, Daniel oth Enthalten in Elsevier Science P-602 - The attitudes of students of high schools in Gjilan related to drug abuse 2012 Amsterdam [u.a.] (DE-627)ELV011183217 volume:56 year:2016 pages:119-131 extent:13 https://doi.org/10.1016/j.apor.2016.01.004 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 33.00 Physik: Allgemeines VZ AR 56 2016 119-131 13 045F 550 |
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Construction of synthetic ocean wave series along the Colombian Caribbean Coast: A wave climate analysis |
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• A methodology was applied to generate synthetic waves series (mean and extreme). • Seasonal variability is generally controlled by trade winds and the hurricane events. • A dipole between the north-east (hurricanes) and the south-west (cold fronts) is found. • During DJF and MAM seasons, in El Niño years low values of wave height occur. • During the JJA season, the highest values occurring during El Niño. |
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• A methodology was applied to generate synthetic waves series (mean and extreme). • Seasonal variability is generally controlled by trade winds and the hurricane events. • A dipole between the north-east (hurricanes) and the south-west (cold fronts) is found. • During DJF and MAM seasons, in El Niño years low values of wave height occur. • During the JJA season, the highest values occurring during El Niño. |
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• A methodology was applied to generate synthetic waves series (mean and extreme). • Seasonal variability is generally controlled by trade winds and the hurricane events. • A dipole between the north-east (hurricanes) and the south-west (cold fronts) is found. • During DJF and MAM seasons, in El Niño years low values of wave height occur. • During the JJA season, the highest values occurring during El Niño. |
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