Anticyclogenesis
AntiCyclogenesis shine ci gaba ko karfafa yaduwar anticyclonic a cikin yanayi. Akasin anticyclolysis ne (rugujewa ko raunana anticyclone) kuma yana da kwatankwacin cyclonic da aka sani da cyclogenesis . [1] Ana kiran anticyclones a madadin Tsarin matsin lamba.
Tsarin
[gyara sashe | gyara masomin]Tsarin matsin lamba mai girma ya samo asali ne saboda motsi zuwa ƙasa ta hanyar troposphere, yanayi yanayi inda yanayi ke faruwa. Yankunan da aka fi so a cikin tsarin kwararar synoptic a matakan da suka fi girma na troposphere suna ƙarƙashin gefen yammacin troughs. A kan taswirar yanayi, waɗannan yankuna suna nuna iskõki masu haɗuwa (isotachs), wanda aka fi sani da haɗuwa, ko layin tsawo masu haɗuwa kusa ko sama da matakin da ba na bambanci ba, wanda ke kusa da matsin lamba na 500 hPa game da tsakiyar hanyar troposphere.[1][2] A kan taswirar yanayi, cibiyoyin matsin lamba suna da alaƙa da harafin H da aka sanya a cikin isobar tare da mafi girman darajar matsin lamba.[3] A kan sigogi na sama na matsin lamba, yana cikin mafi girman layin tsawo.[4]
Dubi kuma
[gyara sashe | gyara masomin]- Anticyclonic storm - Irin guguwa
- Cyclogenesis - Ci gaba ko karfafa yaduwar guguwa a cikin yanayi
- High-pressure area - Yankin da ke da matsin yanayi mafi girma
Manazarta
[gyara sashe | gyara masomin]- ↑ "American Meteorological Society Glossary - Anticyclogenesis". Allen Press Inc. June 2000. Archived from the original on 26 October 2006. Retrieved 2006-11-03.