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The Weather Prediction Center

12. Southern Tropical South America  
Bolivia / Peru / Northern Paraguay / Western and Central Brazil
Graphics use 1° GFS Model Output

ALGORITHM GFS 00Z GFS 12Z
Identification of Surface Fronts - FRONT.CMD
Highlights the positions surface fronts based on horizontal gradients of thickness and dewpoint in the lower troposphere, and precipitable water to a lesser extent. If present, surface fronts are usually positioned in the warm edge of the gradient (thick black contours).
Idle
Idle
Potential for severity and hail - GR02T.CMD
GR02T highlights regions with the potential for severe weather using shades of color, and specifically, detects a potential for hail where colored boxes appear inside colored contours.
Idle
Idle
Enhanced GDI and Flow - EGDI.CMD
Very similar to the GDI, the Enhanced GDI (EGDI) diagnoses the potential for convection and rainfall accumulations. Loops include low- and upper-tropospheric flow and other variables to evaluate if atmospheric dynamics are favorable for triggering and/or sustaining convection.
Idle
(NE South America)

Idle
(Central South America)
Idle
(NE South America)

Idle
(Central South America)
Central Andes Precipitation Accumulation Index - CAPI.CMD
Tool to evaluate the potential for types of precipitation amounts in the central Andes. CAPI is computed using 700-400 hPa mixing ratios (for column moisture content), 600-400 hPa relative humidity and its advection (for dry air entrainment), 700-500 hPa mixing ratio flux convergence and 300-200 hPa divergence (trigger and dynamically-driven ascent), 500-250 hPa shear (preservation of storm structure), and the Lifted Index (deep-layer instability). Boxes appear when the chance of precipitation increases, upon the climatological diurnal cycle of convection. The expected intensity is reflected in colors: green=light, light blue=moderate and fuscia=locally heavy amounts.
Also plotted, the enhanced GDI (>30, >45 and >60 in thick yellow, red and fuscia contours). The flow is the average of 600, 550, 500, 450 and 300 hPa in kt, to evaluate the origin of the air mass entering the Andes, storm cell motion and potential for 'trasvase'/spill over of precipitation into the coast.
Implemented on 27-Jan-2020. Last update: 07-Feb-2020.



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Note: These algorithms are only forecast tools, not official forecasts. For information on the algorithms, click on the red text.


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Page last modified: Thursday, 12-May-2022 19:51:38 UTC