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veering    音标拼音: [v'ɪrɪŋ]
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veering
n 1: the act of turning aside suddenly [synonym: {swerve},
{swerving}, {veering}]

Veer \Veer\, v. i. [imp. & p. p. {Veered}; p. pr. & vb. n.
{Veering}.] [F. virer (cf. Sp. virar, birar), LL. virare;
perhaps fr. L. vibrare to brandish, vibrate (cf. {Vibrate});
or cf. L. viriae armlets, bracelets, viriola a little
bracelet (cf. {Ferrule}). Cf. {Environ}.]
To change direction; to turn; to shift; as, wind veers to the
west or north. "His veering gait." --Wordsworth.
[1913 Webster]

And as he leads, the following navy veers. --Dryden.
[1913 Webster]

an ordinary community which is hostile or friendly as
passion or as interest may veer about. --Burke.
[1913 Webster]

{To veer and haul} (Naut.), to vary the course or direction;
-- said of the wind, which veers aft and hauls forward.
The wind is also said to veer when it shifts with the sun.
[1913 Webster]


Veering \Veer"ing\, a.
Shifting. -- {Veer"ing*ly}, adv.
[1913 Webster]

83 Moby Thesaurus words for "veering":
aberrant, aberrative, broken, capricious, careening, catchy,
choppy, circuitous, departing, desultory, deviant, deviating,
deviative, deviatory, devious, digressive, disconnected,
discontinuous, discursive, eccentric, errant, erratic, excursive,
fitful, flickering, fluctuating, guttering, halting, herky-jerky,
heteroclite, immethodical, inconstant, indirect, intermittent,
intermitting, irregular, jerky, labyrinthine, lurching, mazy,
meandering, nonuniform, out-of-the-way, patchy, planetary,
rambling, rough, roving, scrappy, serpentine, shifting, snaky,
snatchy, spasmatic, spasmic, spasmodic, spastic, sporadic, spotty,
staggering, stray, swerving, turning, twisting, uncertain,
undirected, unequal, uneven, unmethodical, unmetrical, unregular,
unrhythmical, unsettled, unsteady, unsystematic, vagrant, variable,
wandering, wavering, winding, wobbling, wobbly, zigzag


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  • Backing vs Veering Winds (misuse of terms?) | Stormtrack
    A veering wind with height in the lower part of the atmosphere is a type of directional shear often considered important for tornado development -- Also, could someone clearly explain exactly why there is more convergence with backing vs veering winds
  • Veer-back - impacts of backing aloft in supercells | Stormtrack
    Definition of veer-back (-veer) VBV refers to a backing of the winds in a layer above another layer with veering winds, and sometimes bounded above by another layer with veering winds (hence the second -veer in the name) The image below illustrates this feature:
  • Veering vs. Backing winds | Stormtrack
    As a reminder, veering winds with height implies warm-air advection, while backing winds with height (or a backing wind profile) implies cold air advection Typically, in the US, we want to see a veering low-level wind PROFILE (so, veering with height) with a backing surface wind tendency It's also pretty common to see backing winds with height in the mid and upper-levels, which can be
  • Veering (backing) winds and WAA (CAA) | Stormtrack
    Is WAA (CAA) always associated with veering (backing) winds or are there circumstances in which this relationship doesn't hold? I assume the tropics, being highly barotropic, wouldn't see such a relationship but the midlatitudes would due to the high baroclinicity Thanks!
  • Have question regarding veering backing and the cyclonic rotation of . . .
    Now, because a vertically veering wind profile is associated with warm advection at low-levels (e g in the warm sector of a large-scale cyclone), convergence is highest at the southern part of the developing thunderstorm, and so the southern (i e cyclonic) updraught is favoured, and thus tends to become dominant
  • Backing Winds ? | Stormtrack
    The opposite of veering winds In storm spotting, a backing wind usually refers to the turning of a south or southwest surface wind with time to a more east or southeasterly direction Backing of the surface wind can increase the potential for tornado development by increasing the directional shear at low levels
  • Great Lakes Drylines - Stormtrack
    What is striking is the abrupt drop in dewpoints, and again, the veering of surface winds There have been other big tornado days associated with drylines in the Great Lakes region
  • Why does Cold Air Advection cause backing winds with height?
    And, I suspect that the answer will also tell why Warm Air Advection causes veering winds with height I’ve seen this mentioned In multiple basic meteorology resources, but I haven’t seen an explanation of the physics that causes it, and I haven’t been able to intuitively imagine a hypothesis
  • Measuring Shear | Stormtrack
    It's easy to see on a hodograph that you can still have a UNIDIRECTIONAL shear profile even if you have a veering wind profile Most people see se sfc winds at sw flow aloft and think supercells, but that profile can also be one of unidirectional shear (and thus less favoring of cyclonically-rotating supercells)
  • Vorticity | Stormtrack
    In what situations would a veering wind profile produce a straight-line hodograph and unidirectional shear? Would wind speeds have to actually be slower the higher up in the atmosphere you go? There's a great figure in the Markowski and Richardson Mesoscale book to highlight this (Fig 2 13), but I can't find it online





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