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6:17 PM
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2024-12-19

كيف تنشأ حالات عدم الاستقرار الجوي؟ تنشأ حالات عدم الاستقرار عند التقاء هواء بارد في طبقات الجو العليا من الغلاف الجوي مع هواء دافئ أو أكثر حرارة وسخونة في طبقات الجو السفلى. ويتزامن ذلك الالتقاء مع وجود رطوبة كافية في طبقات الجو، لاسيما الطبقات البنائية. وعند حدوث هذا الالتقاء فوق منطقة معينة، تتشكل ما يعرف بالسحب الركامية الرعدية التي تنمو بشكل رأسي في طبقات الجو. وتتميز تلك الحالات بأنها ذات طابع محلي، أي إنها تنشأ السحب داخلياً وتختفي السحب الممطرة في نفس المنطقة المتأثرة بها أو تمتد لمناطق أخرى وتتلاشى بعدها. عماد هذا تعريف عدم الاستقرار هي التقاء منخفض مع اجواء ادفاء ينتج عنها اضطراب جوي اي عدم استقرار

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