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Large-Scale Control on the Patagonian Climate
by
Rojas, M.
, Lopez, P.
, Minvielle, M.
, Garreaud, R.
in
20th century
/ Advection
/ Air temperature
/ Americas
/ Annual variations
/ Anomalies
/ Bgi / Prodig
/ Circulation anomalies
/ Climate
/ Climate change
/ Climate models
/ Climatic zones
/ Climatology
/ Climatology. Bioclimatology. Climate change
/ Cryosphere
/ Dipoles
/ Drying
/ Earth, ocean, space
/ Evaporative
/ Exact sciences and technology
/ External geophysics
/ Glaciers
/ Global climate models
/ Ice
/ Local climates
/ Marine
/ Mathematical models
/ Meteorology
/ Numerical simulations
/ Paleoclimatology
/ Physical geography
/ Precipitation
/ Rainfall
/ Rainfall variability
/ Remote regions
/ Seasons
/ Surface temperature
/ Surface-air temperature relationships
/ Temperate climates
/ Temperate regions
/ Temperature
/ Temperature control
/ Trends
/ Uplift
/ Weather stations
/ Westerly flow
/ Wind
/ Zonal flow
/ Zonal flow (meteorology)
/ Zonal winds
2013
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Large-Scale Control on the Patagonian Climate
by
Rojas, M.
, Lopez, P.
, Minvielle, M.
, Garreaud, R.
in
20th century
/ Advection
/ Air temperature
/ Americas
/ Annual variations
/ Anomalies
/ Bgi / Prodig
/ Circulation anomalies
/ Climate
/ Climate change
/ Climate models
/ Climatic zones
/ Climatology
/ Climatology. Bioclimatology. Climate change
/ Cryosphere
/ Dipoles
/ Drying
/ Earth, ocean, space
/ Evaporative
/ Exact sciences and technology
/ External geophysics
/ Glaciers
/ Global climate models
/ Ice
/ Local climates
/ Marine
/ Mathematical models
/ Meteorology
/ Numerical simulations
/ Paleoclimatology
/ Physical geography
/ Precipitation
/ Rainfall
/ Rainfall variability
/ Remote regions
/ Seasons
/ Surface temperature
/ Surface-air temperature relationships
/ Temperate climates
/ Temperate regions
/ Temperature
/ Temperature control
/ Trends
/ Uplift
/ Weather stations
/ Westerly flow
/ Wind
/ Zonal flow
/ Zonal flow (meteorology)
/ Zonal winds
2013
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Do you wish to request the book?
Large-Scale Control on the Patagonian Climate
by
Rojas, M.
, Lopez, P.
, Minvielle, M.
, Garreaud, R.
in
20th century
/ Advection
/ Air temperature
/ Americas
/ Annual variations
/ Anomalies
/ Bgi / Prodig
/ Circulation anomalies
/ Climate
/ Climate change
/ Climate models
/ Climatic zones
/ Climatology
/ Climatology. Bioclimatology. Climate change
/ Cryosphere
/ Dipoles
/ Drying
/ Earth, ocean, space
/ Evaporative
/ Exact sciences and technology
/ External geophysics
/ Glaciers
/ Global climate models
/ Ice
/ Local climates
/ Marine
/ Mathematical models
/ Meteorology
/ Numerical simulations
/ Paleoclimatology
/ Physical geography
/ Precipitation
/ Rainfall
/ Rainfall variability
/ Remote regions
/ Seasons
/ Surface temperature
/ Surface-air temperature relationships
/ Temperate climates
/ Temperate regions
/ Temperature
/ Temperature control
/ Trends
/ Uplift
/ Weather stations
/ Westerly flow
/ Wind
/ Zonal flow
/ Zonal flow (meteorology)
/ Zonal winds
2013
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Journal Article
Large-Scale Control on the Patagonian Climate
2013
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Overview
Patagonia, located in southern South America, is a vast and remote region holding a rich variety of past environmental records but a small number of meteorological stations. Precipitation over this region is mostly produced by disturbances embedded in the westerly flow and is strongly modified by the austral Andes. Uplift on the windward side leads to hyperhumid conditions along the Pacific coast and the western slope of the Andes; in contrast, downslope subsidence dries the eastern plains leading to arid, highly evaporative conditions.
The authors investigate the dependence of Patagonia’s local climate (precipitation and near-surface air temperature) year-to-year variability on large-scale circulation anomalies using results from a 30-yr-long high-resolution numerical simulation. Variations of the low-level zonal wind account for a large fraction of the rainfall variability at synoptic and interannual time scales. Zonal wind also controls the amplitude of the air temperature annual cycle by changing the intensity of the seasonally varying temperature advection.
The main modes of year-to-year variability of the zonal flow over southern South America are also investigated. Year round there is a dipole between mid- and high latitudes. The node separating wind anomalies of opposite sign migrates through the seasons, leading to a dipole over Patagonia during austral summer and a monopole during winter. Reanalysis data also suggests that westerly flow has mostly decreased over north-central Patagonia during the last four decades, causing a drying trend to the west of the Andes, but a modest increase is exhibited over the southern tip of the continent.
Publisher
American Meteorological Society
Subject
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