Maksud "hazy" dalam kamus Corsica

Jerebu secara tradisi merupakan fenomena atmosfer di mana habuk, asap dan zarah kering lain mengaburkan kejelasan langit. Manual Pertubuhan Meteorologi Dunia kod mengandungi sekumpulan pengikisan mendatar ke dalam kategori kabus, kabut ais, kabut stim, kabus, kabut, asap, abu gunung berapi, habuk, pasir dan salji. Sumber untuk zarah kabus termasuk pertanian, trafik, industri, dan kebakaran hutan. Dilihat dari jauh dan bergantung kepada arah pandangan berkenaan dengan matahari, jerebu boleh kelihatan berwarna kecoklatan atau kebiruan, sementara kabut cenderung berwarna abu-abu kebiruan. Manakala jerebu sering dianggap sebagai fenomena udara kering, pembentukan kabus adalah fenomena udara lembap. Walau bagaimanapun, zarah kabus boleh bertindak sebagai nukleus pemeluwapan untuk pembentukan titisan kabus yang kemudiannya; bentuk jerebu seperti "jerebu basah." Di Amerika Syarikat dan di tempat lain, istilah "jerebu" dalam kesusasteraan meteorologi umumnya digunakan untuk menunjukkan aerosol pengurangan ketahanan jenis basah. Aerosol sedemikian biasanya timbul daripada tindak balas kimia kompleks yang berlaku apabila gas sulfur dioksida yang dikeluarkan semasa pembakaran ditukar kepada titisan kecil asid sulfurik. Haze is traditionally an atmospheric phenomenon where dust, smoke and other dry particles obscure the clarity of the sky. The World Meteorological Organization manual of codes includes a classification of horizontal obscuration into categories of fog, ice fog, steam fog, mist, haze, smoke, volcanic ash, dust, sand and snow. Sources for haze particles include farming, traffic, industry, and wildfires. Seen from afar and depending upon the direction of view with respect to the sun, haze may appear brownish or bluish, while mist tends to be bluish-grey. Whereas haze often is thought of as a phenomenon of dry air, mist formation is a phenomenon of humid air. However, haze particles may act as condensation nuclei for the subsequent formation of mist droplets; such forms of haze are known as "wet haze." In the United States and elsewhere, the term "haze" in meteorological literature generally is used to denote visibility-reducing aerosols of the wet type. Such aerosols commonly arise from complex chemical reactions that occur as sulfur dioxide gases emitted during combustion are converted into small droplets of sulfuric acid.