- Teks
- Sejarah
When the NAO is strongly negative (
When the NAO is strongly negative (Fig. 9.06b), the Icelandic low is weaker,
less persistent, and located further south. It brings relatively warm easterly winds to the Labrador Sea. At the same time, colder northerly winds are blowing
over the Greenland Sea. The westerlies in the North Atlantic are weaker, so
that northern Europe is colder than normal. The Azores high is also weaker, with
lower wind speeds and decreased upwelling off the northwest African coast.
less persistent, and located further south. It brings relatively warm easterly winds to the Labrador Sea. At the same time, colder northerly winds are blowing
over the Greenland Sea. The westerlies in the North Atlantic are weaker, so
that northern Europe is colder than normal. The Azores high is also weaker, with
lower wind speeds and decreased upwelling off the northwest African coast.
0/5000
When the NAO is strongly negative (Fig. 9.06b), the Icelandic low is weaker,less persistent, and located further south. It brings relatively warm easterly winds to the Labrador Sea. At the same time, colder northerly winds are blowingover the Greenland Sea. The westerlies in the North Atlantic are weaker, sothat northern Europe is colder than normal. The Azores high is also weaker, withlower wind speeds and decreased upwelling off the northwest African coast.
Sedang diterjemahkan, harap tunggu..
Ketika NAO adalah sangat negatif (Gambar. 9.06b), rendah Islandia adalah lemah,
kurang gigih, dan terletak di sebelah selatan lebih lanjut. Ini membawa angin timur yang relatif hangat ke Laut Labrador. Pada saat yang sama, angin dingin dari utara bertiup
di atas Laut Greenland. Baratan di Atlantik Utara yang lemah, sehingga
bahwa Eropa Utara lebih dingin dari biasanya. Azores tinggi juga lemah, dengan
kecepatan angin lebih rendah dan penurunan upwelling di lepas pantai Afrika barat laut.
kurang gigih, dan terletak di sebelah selatan lebih lanjut. Ini membawa angin timur yang relatif hangat ke Laut Labrador. Pada saat yang sama, angin dingin dari utara bertiup
di atas Laut Greenland. Baratan di Atlantik Utara yang lemah, sehingga
bahwa Eropa Utara lebih dingin dari biasanya. Azores tinggi juga lemah, dengan
kecepatan angin lebih rendah dan penurunan upwelling di lepas pantai Afrika barat laut.
Sedang diterjemahkan, harap tunggu..
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