PowerPoint Presentation · isentropic ascent isentropic descent l pressure wind isentropic ascent...

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Transcript of PowerPoint Presentation · isentropic ascent isentropic descent l pressure wind isentropic ascent...

Page 1: PowerPoint Presentation · isentropic ascent isentropic descent l pressure wind isentropic ascent (positive p advection) isentropic descent (negative p advection) isentropic analysis.
Page 2: PowerPoint Presentation · isentropic ascent isentropic descent l pressure wind isentropic ascent (positive p advection) isentropic descent (negative p advection) isentropic analysis.
Page 3: PowerPoint Presentation · isentropic ascent isentropic descent l pressure wind isentropic ascent (positive p advection) isentropic descent (negative p advection) isentropic analysis.
Page 4: PowerPoint Presentation · isentropic ascent isentropic descent l pressure wind isentropic ascent (positive p advection) isentropic descent (negative p advection) isentropic analysis.

17 ° LAT. S

69 ° LONG. W

Page 5: PowerPoint Presentation · isentropic ascent isentropic descent l pressure wind isentropic ascent (positive p advection) isentropic descent (negative p advection) isentropic analysis.

300 FAMILIES AFFECTED

BY DRIZZLE

160 FAMILIES

AFFECTED BY RAIN

CLOSED BORDER

CROSSING

Page 6: PowerPoint Presentation · isentropic ascent isentropic descent l pressure wind isentropic ascent (positive p advection) isentropic descent (negative p advection) isentropic analysis.

SCFA

1.5mm

UCN : O.5 mm

TS DUST

GUSTS

45 KT 60KT

SCAT 1.6MM

6 mm

Canto del agua 6.5mm

JUNTA DEL CARMEN

4.5mm

EMBALSE SANTA JUANA

3.8MM

3mm

JUNTA DEL CARMEN 4.5mm

PASO

SAN

FRANCISCO N. Anto: 0.5mm

N. Vall: 2,1mm

Page 7: PowerPoint Presentation · isentropic ascent isentropic descent l pressure wind isentropic ascent (positive p advection) isentropic descent (negative p advection) isentropic analysis.

LEFT ENTRANCE

RIGHT EXIT

• JET STREAM (ISOTACHS)

• UPPER DIVERGENCE

• ADV. CYCLONIC VORTICITY

• GEOP. DROPS OF 80MGP/DAY

X

JET MAX

Page 8: PowerPoint Presentation · isentropic ascent isentropic descent l pressure wind isentropic ascent (positive p advection) isentropic descent (negative p advection) isentropic analysis.

ISENTROPIC ASCENT

ISENTROPIC DESCENT

L

PRESSURE

WIND

ISENTROPIC ASCENT (POSITIVE P ADVECTION)

ISENTROPIC DESCENT (NEGATIVE P ADVECTION)

ISENTROPIC ANALYSIS.

Page 9: PowerPoint Presentation · isentropic ascent isentropic descent l pressure wind isentropic ascent (positive p advection) isentropic descent (negative p advection) isentropic analysis.

(1) 500HPA WIND >50 KT (2) WEAKENING OF DIURNAL

CYCLE AT CALAMA

ANTOFAGASTA (COAST) CALAMA ( FOOTHILLS)

SE W SE W W W

DU

ST

ST

OR

M

DU

ST

ST

OR

M

Page 10: PowerPoint Presentation · isentropic ascent isentropic descent l pressure wind isentropic ascent (positive p advection) isentropic descent (negative p advection) isentropic analysis.

COAST

ANDES

MOUNTAINS

• POTENTIAL

TEMPERATURE [K]

• SATURATION ( RH)

[%]

• WIND [kt]

• TOPOGRAPHY

CROSS SECTION IN ANTOFAGASTA

Page 11: PowerPoint Presentation · isentropic ascent isentropic descent l pressure wind isentropic ascent (positive p advection) isentropic descent (negative p advection) isentropic analysis.

ANDES

MOUNTAINS

COST

• WIND (kt)

• CONV.

• SATURATION ( HR)

• ( % )

• POTENTIAL

TEMPERATURE ( K)

• TOPOGRAPY

CROSS SECTION IN ATACAMA REGION

Page 12: PowerPoint Presentation · isentropic ascent isentropic descent l pressure wind isentropic ascent (positive p advection) isentropic descent (negative p advection) isentropic analysis.

SCFA

SCAT

SCCF

PASO SAN

FRANCISCO.

Page 13: PowerPoint Presentation · isentropic ascent isentropic descent l pressure wind isentropic ascent (positive p advection) isentropic descent (negative p advection) isentropic analysis.

SCFA SCCF

SCAT PASO SAN

FRANCISCO

Page 14: PowerPoint Presentation · isentropic ascent isentropic descent l pressure wind isentropic ascent (positive p advection) isentropic descent (negative p advection) isentropic analysis.

• Based on the application of the tools learned in the Sudamerican Desk:

• GFS model variables were sufficient to detect and forecast the event.

• Contribute to the creation of an early warning system (ONEMI*).

*ONEMI: National emergency office.