Hydrology & Fluid Dynamics Faculty Database
Hydrology & Fluid Dynamics
Pratt School of Engineering
Duke University

 HOME > pratt > CEE_HFD > Faculty    Search Help Login 

Publications [#282779] of Ana P. Barros

Papers Published

  1. Lang, TJ; Barros, AP, Winter storms in the central Himalayas, Journal of the Meteorological Society of Japan. Ser. Ii, vol. 82 no. 3 (June, 2004), pp. 829-844, Meteorological Society of Japan [doi]
    (last updated on 2023/06/01)

    Abstract:
    Based on observations from a hydrometeorological network on the eastern slopes of the Annapurna Range, nearly all the annual precipitation at low elevations (< 2000 in MSL) in Nepal is in liquid form, even during the winter. However, high elevations (> 3000 in MSL) can receive up to 40% of their annual precipitation as snowfall during the winter, with the highest altitude stations (∼4000 m MSL and above) having the most total winter precipitation (which can exceed 100 cm). Significant snowstorms are associated with terrain-locked low-pressure systems that form when an upper-level disturbance passes over the notch formed by the Himalayas and Hindu Kush mountains (the so-called Western Disturbances), causing upper-level SW flow over central Nepal and orographically forced precipitation. Based on these results, a 30-year (1973-2002) climatology of these notch depressions is developed and reveals that significant interannual variability in central Himalayan winter storms exists. Weak but statistically significant correlation between notch depressions and the Polar/Eurasia teleconnection pattern was found, suggesting that the strength of the circumpolar vortex may affect the number of depressions passing through the Himalayan region. A typical snow event (11 February 2000) was the subject of an observational and modeling case study. Local precipitation (snow and rain) and other meteorological observations, as well as satellite (Meteosat-5 and TRMM) and NCEP/NCAR Reanalysis data were used, along with a cloud-resolving model with realistic topography. This study shows that significant winter-time precipitation only occurs in the central Himalayas when the large-scale flow evolves to a favorable geometry with respect to the mountains. © 2004, Meteorological Society of Japan.


Duke University * Pratt * Faculty * Reload * Login
x