Εξώφυλλο

Μελέτη του κυκλώνα Λάουρα στον Τροπικό βόρειο Ατλαντικό ωκεανό το 2020 = Study of hurricane Laura in the tropical north Atlantic ocean in 2020

Εμμανουήκ Εδουάρδος Σερμανουκιάν

Περίληψη


Κύριο στόχο της διπλωματικής εργασίας αποτελεί η περιγραφή και ανάλυση του τροπικού συστήματος που οδήγησε στη δημιουργία του κυκλώνα Λάουρα στον βόρειο Ατλαντικό ωκεανό το 2020.Για τον σκοπό αυτό συνδυάστηκαν δορυφορικά,
πραγματικά δεδομένα μαζί με πλεγματικά δεδομένα αναδρομικών αναλύσεων ERA5.
Μελετήθηκε η εξέλιξη ενός Αφρικανικού ανατολικού κύματος στον κυκλώνα Λάουρα πάνω από τον Ατλαντικό ωκεανό κατά την διάρκεια της εποχής των κυκλώνων τον Αύγουστο του 2020. Εντοπίστηκε η ύπαρξη ενός αφρικανικού ανατολικού κύματος
στην τροπική ΒΔ Αφρική. Μέσω του Αφρικανικού ανατολικού αεροχείμμαρου κινήθηκε γενικά δυτικά πάνω από τον τροπικό ΒΑ Ατλαντικό ωκεανό. Οι κατάλληλες περιβαλλοντικές και ατμοσφαιρικές συνθήκες πάνω από τον Β Ατλαντικό ωκεανό ήταν
αυτές που τελικά ευνόησαν στην περεταίρω ενίσχυση του συστήματος σε τροπική ύφεση και τροπική καταιγίδα. Τέλος, η ύπαρξη πολύ θερμών επιφανειακών νερών ιδιαίτερα εντός του Κόλπου του Μεξικού ευνόησαν την αναβάθμιση του συστήματος
στον κυκλώνα Λάουρα. Η σύγκριση των πραγματικών δεδομένων με τις αναδρομικές αναλύσεις ERA5 έδειξε ότι οι τελευταίες δεν μπόρεσαν να αποτυπώσουν την πλήρη ένταση του κυκλώνα.

The main aim of this bachelor thesis is the description and analysis of the tropical system that created hurricane Laura in north Atlantic in 2020. For this purpose meteorological measurements, satellite data and ERA5 reanalysis data were combined and processed.
The evolution of an African Easterly Wave in hurricane Laura over the Atlantic ocean during the August 2020 hurricane season was examined. An African Easterly Wave was detected in tropical NW Africa. Through the African easterly jet it moved generally westward over the tropical NE Atlantic ocean. The favorable environmental and atmospheric conditions over the N Atlantic ocean were ultimately conductive to the further strengthening of the system into a tropical depression and tropical storm. Finally, the occurrence of warm sea surface waters particularly within the Gulf of Mexico contributed significantly to the upgrade of the system to hurricane Laura. The comparison of the actual data with the ERA5 reanalyses  showed that the gridded data did not manage to represent the actual intensity of the hurricane.

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Αναφορές


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