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Shapiro, M. A., 1984: Meteorological tower measurements of a surface cold front. Mon. Wea. Rev., 112, 1634-1639. Shapiro (1984)

Jan 16, 2016

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Page 1: Shapiro, M. A., 1984: Meteorological tower measurements of a surface cold front. Mon. Wea. Rev., 112, 1634-1639. Shapiro (1984)
Page 2: Shapiro, M. A., 1984: Meteorological tower measurements of a surface cold front. Mon. Wea. Rev., 112, 1634-1639. Shapiro (1984)

Shapiro, M. A., 1984: Meteorological tower measurements of a surface cold front. Mon. Wea. Rev., 112, 1634-1639.

Shapiro (1984)

Page 3: Shapiro, M. A., 1984: Meteorological tower measurements of a surface cold front. Mon. Wea. Rev., 112, 1634-1639. Shapiro (1984)

BAO tower

WNW downslope

flow

Temperatures (°C)winds (barb = 10 kts)

The passage of a strong cold front in eastern Colorado

We will be interested in the structure of this front as it passes the

Boulder Atmospheric Observatory tower

Page 4: Shapiro, M. A., 1984: Meteorological tower measurements of a surface cold front. Mon. Wea. Rev., 112, 1634-1639. Shapiro (1984)

The Boulder Atmospheric Observatory Tower located in Erie, Colorado near I-25

Page 5: Shapiro, M. A., 1984: Meteorological tower measurements of a surface cold front. Mon. Wea. Rev., 112, 1634-1639. Shapiro (1984)

Cross section of the cold front that passed the BAO tower on 24 March 1982

Based on a rawinsonde at Denver, a radiometer temperature profile, a lidar wind profile and surface data

Page 6: Shapiro, M. A., 1984: Meteorological tower measurements of a surface cold front. Mon. Wea. Rev., 112, 1634-1639. Shapiro (1984)

Potential temperature (K, solid) and front normal wind component (m/s, dashed)

Two minutes!!!

300 meters

superadiabaticlapse rate

Page 7: Shapiro, M. A., 1984: Meteorological tower measurements of a surface cold front. Mon. Wea. Rev., 112, 1634-1639. Shapiro (1984)

Vertical motion (m/s) measured by sonic anemometers on the tower

Frontal boundaries denoted by solid lines

Page 8: Shapiro, M. A., 1984: Meteorological tower measurements of a surface cold front. Mon. Wea. Rev., 112, 1634-1639. Shapiro (1984)

zy

w

xy

u

yy

v

ydt

d

Miller 2-D frontogenesis function (neglecting diabatic processes and turbulence)

Change in potentialtemperature gradient

following parcel

Confluenceacting ongradient

Shearacting ongradient

Tilting of verticalgradient

Can’t evaluate this -so assume negligiblebased on surface data

Do the flow fields suggest that frontal contraction was occurring at the time the front passed the tower?

Page 9: Shapiro, M. A., 1984: Meteorological tower measurements of a surface cold front. Mon. Wea. Rev., 112, 1634-1639. Shapiro (1984)

Miller 2-D frontogenesis function (neglecting diabatic processes and turbulence)

Change in potentialtemperature gradient

following parcel

Confluenceacting ongradient

Shearacting ongradient

Tilting of verticalgradient

confluence term

zy

w

xy

u

yy

v

ydt

d

Page 10: Shapiro, M. A., 1984: Meteorological tower measurements of a surface cold front. Mon. Wea. Rev., 112, 1634-1639. Shapiro (1984)

Miller 2-D frontogenesis function (neglecting diabatic processes and turbulence)

Change in potentialtemperature gradient

following parcel

Confluenceacting ongradient

Shearacting ongradient

Tilting of verticalgradient

Tilting term

zy

w

xy

u

yy

v

ydt

d

Page 11: Shapiro, M. A., 1984: Meteorological tower measurements of a surface cold front. Mon. Wea. Rev., 112, 1634-1639. Shapiro (1984)

Miller 2-D frontogenesis function (neglecting diabatic processes and turbulence)

Change in potentialtemperature gradient

following parcel

Confluenceacting ongradient

Shearacting ongradient

Tilting of verticalgradient

Total frontogenesis

0

0

ydt

d

ydt

d

Frontolytical

Frontogenetical

zy

w

xy

u

yy

v

ydt

d