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anticycloni
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The answer ANTICYCLONI has 0 possible clue(s) in existing crosswords.
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The word ANTICYCLONI is NOT valid in any word game. (Sorry, you cannot play ANTICYCLONI in Scrabble, Words With Friends etc)
There are 11 letters in ANTICYCLONI ( A1C3I1L1N1O1T1Y4 )
To search all scrabble anagrams of ANTICYCLONI, to go: ANTICYCLONI?
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Scrabble results that can be created with an extra letter added to ANTICYCLONI
10 letters out of ANTICYCLONI
8 letters out of ANTICYCLONI
7 letters out of ANTICYCLONI
6 letters out of ANTICYCLONI
5 letters out of ANTICYCLONI
ACINI
ACTIN
AIOLI
ALOIN
ANCON
ANION
ANNOY
ANTIC
ANYON
ATONY
CACTI
CANNY
CANON
CANTO
CANTY
CILIA
COACT
COALY
COATI
COLIC
COLIN
CONIC
CONIN
COTAN
CYANO
CYCLO
CYNIC
CYTON
ICILY
ICTIC
ILIAC
INION
INLAY
IONIC
LAITY
LAYIN
LICIT
LINAC
LININ
LINTY
LITAI
LOTIC
LYTIC
NANCY
NICOL
NITON
NOILY
NONYL
NOTAL
NYLON
OCTAL
OCTAN
OCTYL
ONLAY
ONTIC
TALON
TICAL
TINNY
TOLAN
TONAL
TONIC
YONIC
4 letters out of ANTICYCLONI
ACYL
ALIT
ALTO
ANIL
ANON
ANTI
AYIN
CAIN
CALO
CANT
CIAO
CION
CITY
CLAN
CLAY
CLON
CLOT
CLOY
COAL
COAT
COCA
COIL
COIN
COLA
COLT
COLY
CONI
CONN
CONY
CYAN
ICON
ILIA
INIA
INLY
INTI
INTO
IOTA
LACY
LAIC
LAIN
LATI
LINN
LINO
LINT
LINY
LION
LOAN
LOCA
LOCI
LOIN
LOTA
LOTI
NAIL
NAOI
NOIL
NONA
NOTA
OILY
ONLY
OTIC
TACO
TAIL
TAIN
TALC
TALI
TINY
TOIL
TOLA
TONY
TYIN
YONI
3 letters out of ANTICYCLONI
Searching in Dictionaries ...
Definitions of anticycloni in various dictionaries:
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Anticycloni might refer to |
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An Anticyclone (that is, opposite to a cyclone) is a weather phenomenon defined by the United States National Weather Service's glossary as "a large-scale circulation of winds around a central region of high atmospheric pressure, clockwise in the Northern Hemisphere, counterclockwise in the Southern Hemisphere". Effects of surface-based anticyclones include clearing skies as well as cooler, drier air. Fog can also form overnight within a region of higher pressure. Mid-tropospheric systems, such as the subtropical ridge, deflect tropical cyclones around their periphery and cause a temperature inversion inhibiting free convection near their center, building up surface-based haze under their base. Anticyclones aloft can form within warm core lows such as tropical cyclones, due to descending cool air from the backside of upper troughs such as polar highs, or from large scale sinking such as the subtropical ridge. * The evolution of an anticyclone depends on a few variables such as its size, intensity, moist-convection, Coriolis force etc . |