Atmospheric circulation over the Bolivian Altiplano during ... - CDAM

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1586M. VUILLEFigures 4 and 5 show the same analysis based on monthly NCEP reanalysis data. Although monthlydata might mask some of the differences between dry and wet periods, which last only a few days, theresults are in good agreement with those obtained from the daily radiosonde data. Figure 4(a–c) showsthe easterly wind anomalies during WET, when compared to DRY. These anomalies become moresignificant with increasing height. At the 200 hPa level easterly anomalies dominate over the entirePeru–Bolivian Altiplano (Figure 4(c)). The geopotential height difference in Figure 4(e–f) also confirmsthe radiosonde data, by featuring an increase at mid- and upper-tropospheric levels over the southernFigure 3. WET-DRY summer (DJF) composite from daily radiosonde data for: (a) zonal wind component (m s −1 ); (b) meridionalwind component (m s −1 ); (c) geopotential height (gpm); (d) air temperature (°C); and (e) specific humidity (g kg −1 ) overAntofagasta, Salta, Lima and La Paz. Filled markers indicate significant difference at the 95% level between WET and DRYcompositeCopyright © 1999 Royal Meteorological Society Int. J. Climatol. 19: 1579–1600 (1999)
BOLIVIAN DRY AND WET PERIODS AND CIRCULATION 1587Figure 4. WET-DRY summer (DJF) composite from monthly NCEP reanalysis data showing: (a) windfield at 850 hPa (m s −1 ); (b)as in (a) but for 500 hPa; (c) as in (a) but for 200 hPa; (d) geopotential height (gpm) at 850 hPa; (e) as in (d) but for 500 hPa; (f)as in (d) but for 200 hPa; (g) air temperature (°C) for 850 hPa; (h) as in (g) but for 500 hPa; and (i) as in (g) but for 200 hPa.Negative contour lines are dashed. Shaded grid boxes indicate areas with significant difference at the 95% level between WET andDRY composite. At the 850 hPa level ((a), (d) and (g)), the Andes are superimposed on the NCEP data as the shaded area above3000 mAltiplano and a decrease over the northern part of the study area. Although the difference between WETand DRY is significant in the northern part and at the 200 hPa level only, the pattern confirms the notionof a southward displaced Bolivian High. This displacement is also evident in the individual WET andDRY composites (not shown). Temperature is lowered during WET as compared to DRY over the entirestudy area at the 200 hPa level (Figure 4(i)), and over the northern part at the 500 hPa level (Figure 4(h)),consistent with the radiosonde data (see Figure 3(d)). An additional measure in terms of the origin of thehumidity is provided by the computation of the water vapour flux. Figure 5 shows the water vapourtransport over the Altiplano during WET (Figure 5(a–c)) and DRY (Figure 5(d–f)) at the 700, 500 and300 hPa level. To simplify the interpretation, the actual DRY and WET composites are shown, ratherthan the difference between the two. Note that Figure 5 is zoomed in and shows a smaller region(10°S–25°S; 75°W–55°W) than Figure 4. Both the 500 and the 300 hPa level show a strengthenedCopyright © 1999 Royal Meteorological Society Int. J. Climatol. 19: 1579–1600 (1999)
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Atmospheric circulation over the Bolivian Altiplano during ... - CDAM

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