chapter 2 Flashcards
The Mediterranean Basin (MB) is one of the most
cyclogenetic regions in the world.
The Mediterranean Basin (MB) is one of the most cyclogenetic regions in the world. This is in spite of its being
south of the global mid-latitude cyclone belt and the fact that its southern end, latitude 30◦N, denotes the northern border of the global desert belt.
The southern location of the MB suppresses
cyclonic activity in the summer, leaving the winter as the main active season.
In the winter, the MB offers all the cyclogenetic factors, being
- highly baroclinic,
- warmer than its surroundings and
- positioned at the lee of mountain ridges, such as the Atlas ridge in Morocco, the European Alps and the Taurus ridge in Turkey.
جبال الاطلس في المغرب
جبال الالب في اوروبا
جبال توروس في تركيا
The MB winter cyclones have some special characteristics:
- they develop mainly at the northern Mediterranean coasts
- their horizontal size varies between meso-scale and synoptic-scale;
- their life span is around one to four days;
- their typical speed is ∼5 ms−1.
In addition to the winter cyclones, another type of frontal cyclone, known as the
“Sharav”, or “North African Cyclone”, is observed in the MB.
“Sharav”, or “North African Cyclone”, is observed in the MB. These cyclones, most frequent in the
spring season
“Sharav”, or “North African Cyclone”, is observed in the MB. These cyclones, most frequent in the spring season, develop and move along the
southern coast of the MB.
“Sharav”, or “North African Cyclone”, is observed in the MB. These cyclones, most frequent in the spring season, develop and move along the southern coast of the MB. They owe their existence to
the high temperature gradient that develops between the Mediterranean Sea and the African continent during that season.
The winter cyclone track in the MB co-exists with the
European track
The winter cyclone track in the MB co-exists with the European track, which is an extension of the
Atlantic stormtrack
The winter cyclone track in the MB co-exists with the European track, which is an extension of the Atlantic stormtrack. It is therefore possible that
the MB cyclones are influenced by the European ones.
Main winter cyclone track in the MB.
The main track is
eastward, along the northern coast of the Mediterranean, down to the Levant region, with three branches
The main track is eastward, along the northern coast of the Mediterranean, down to the Levant region, with three branches toward
northeast, where cyclones leave the MB in favor of the European track
The main track is eastward, along the northern coast of the Mediterranean, down to the Levant region, with three branches toward the northeast, where cyclones leave the MB in favor of the European track;
two in the Adriatic Sea (ITALY) and one in the Aegean Sea (Grees). An additional track extends from the lee of the Atlas along the North Africa coast.