Meteorological Interpretation of Orographic Precipitation Gradients along an Andes West Slope Basin at 30°S (Elqui Valley, Chile)

• Published in: Journal of hydrometeorology 2017-03, Vol.18 (3), p.713-727
• Main Authors: Scaff, Lucia, Rutllant, Jose A., Rahn, David, Gascoin, Simon, Rondanelli, Roberto
• Format: Article
• Language: English
• Subjects: Altitude; Ascent; Atmospheric precipitations; Coastal zone; Continental interfaces, environment; Cyclones; Froude number; Gauges; Hydrology; Migration; Mountain regions; Mountainous areas; Orographic precipitation; Precipitation; Precipitation measurements; Rain; Rainfall; Resource availability; Sciences of the Universe; Snow; Snow accumulation; Static stability; Storms; Stream discharge; Stream flow; Streamflow forecasting; Studies; Topography; Topography (geology); Valleys; Vertical stability; Water resources; Westerlies; Winds; Zonal winds
• ISSN: 1525-755X; 1525-7541
• DOI: 10.1175/JHM-D-16-0073.1

To better forecast streamflow and water resource availability, it is important to have an understanding of the meteorological drivers of the orographic precipitation gradient (OPG), especially critical in semiarid mountainous areas. Although forced ascent over topography typically results in precipitation increasing with altitude (positive OPGs), mean annual OPGs and especially OPGs associated with individual storms can change widely in magnitude and even sign. Precipitation measurements from the Elqui Valley in the semiarid Andes of Chile (30°S) reveal a mean annual OPG of 6.3 mm km−1 (millimeters of precipitation over kilometers in elevation) ranging from −42 to 52 mm km−1 for individual storms over the last 35 years (1979–2013). Reanalysis data and precipitation measurements are used to characterize the observed OPG in this region in relation with their synoptic-scale flow. It is found that the Froude number correlates positively with the OPG, reflecting stronger zonal winds and less static stability during storms that have positive OPGs. Altitude of the Andes barrier jet shows only a weak relationship with the OPG. Significant storms with positive OPGs are typically linked with an austral blocking of the westerlies and an equatorward migration of the midlatitude storm track. For negative OPGs, either a cutoff low or the northern edge of a surface migratory cyclone reaches the Elqui Valley in such a way that significant rainfall only occurs in the near-coastal region without major snowfall accumulation over the Andes.