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A Case Study of a Chaco Low-Level Jet Event

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What this work says

Outgoing claims: the papers this work cites, builds on, or argues with.

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Tropical-midlatitude exchange of air masses during summer and winter in South America: climatic aspects and examples of intense events
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The seasonal mean flow and distribution of large-scale weather systems in the southern hemisphere: the effects of moisture transports
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Model characterization of the South American low-level flow during the 1997-1998 spring-summer season
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The effect of the low-level jet on the poleward water vapour transport in the central region of South America
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Computational Design of the Basic Dynamical Processes of the UCLA General Circulation Model
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The South American low‐level jet east of the Andes during the 1999 LBA‐TRMM and LBA‐WET AMC campaign
inferredcites →https://doi.org/10.1029/2001jd001315openalex-snapshot
Chaco low‐level jet events characterization during the austral summer season
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The diurnal boundary layer wind oscillation above sloping terrain
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The New NMC Mesoscale Eta Model: Description and Forecast Examples
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Importance of Low-Level Jets to Climate: A Review
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Large-Scale Atmospheric Moisture Cycling As Evaluated from NMC Global Analysis and Forecast Products
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Does a Monsoon Climate Exist over South America?
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Climatology of the Low-Level Jet East of the Andes as Derived from the NCEP–NCAR Reanalyses: Characteristics and Temporal Variability
inferredcites →https://doi.org/10.1175/1520-0442(2004)017<3829:svoris>2.0.co;2openalex-snapshot
Subseasonal Variations of Rainfall in South America in the Vicinity of the Low-Level Jet East of the Andes and Comparison to Those in the South Atlantic Convergence Zone
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A Parameterization for the Absorption of Solar Radiation in the Earth's Atmosphere
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A Hierarchy of Turbulence Closure Models for Planetary Boundary Layers
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The Simplified Exchange Approximation: A New Method for Radiative Transfer Calculations
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Parameterization of the Dynamics of Stable Boundary Layers and Nocturnal Jets
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Diurnal Boundary-Layer Development over Sloping Terrain
inferredcites →https://doi.org/10.1175/1520-0477-38.5.283openalex-snapshot
Boundary Layer Wind Maxima and Their Significance for the Growth of Nocturnal Inversions
inferredcites →https://doi.org/10.1175/1520-0493(1968)096<0833:cotllj>2.0.co;2openalex-snapshot
CLIMATOLOGY OF THE LOW LEVEL JET
inferredcites →https://doi.org/10.1175/1520-0493(1970)098<0735:dviblw>2.3.co;2openalex-snapshot
DIURNAL VARIATIONS IN BOUNDARY LAYER WINDS OVER THE SOUTH-CENTRAL UNITED STATES IN SUMMER
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The Coupling of Upper and Lower Tropospheric Jet Streaks and Implications for the Development of Severe Convective Storms
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Diurnal Oscillations of Low-Level Jets, Vertical Motion, and Precipitation: A Model Case Study
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The Step-Mountain Eta Coordinate Model: Further Developments of the Convection, Viscous Sublayer, and Turbulence Closure Schemes
inferredcites →https://doi.org/10.1175/1520-0493(1994)122<2257:adsotl>2.0.co;2openalex-snapshot
A Diagnostic Study of the Low-Level Jet during TAMEX IOP 5
inferredcites →https://doi.org/10.1175/1520-0493(1997)125<0279:awadco>2.0.co;2openalex-snapshot
Alternating Wet and Dry Conditions over South America during Summer
inferredcites →https://doi.org/10.1175/1520-0493(1997)125<1931:apcsfo>2.0.co;2openalex-snapshot
A Prognostic Cloud Scheme for Operational NWP Models
inferredcites →https://doi.org/10.1175/1520-0493(1998)126<2972:lljdda>2.0.co;2openalex-snapshot
Low-Level Jet Development during a Numerically Simulated Return Flow Event
inferredcites →https://doi.org/10.1175/1520-0493(2000)128<1328:spawvf>2.0.co;2openalex-snapshot
Springtime Precipitation and Water Vapor Flux over Southeastern South America
inferredcites →https://doi.org/10.1175/1520-0493(2002)130<0059:cfpvmt>2.0.co;2openalex-snapshot
Cold-Frontal Potential Vorticity Maxima, the Low-Level Jet, and Moisture Transport in Extratropical Cyclones
inferredcites →https://doi.org/10.1175/1520-0493(2003)131<2361:tnalas>2.0.co;2openalex-snapshot
The Northwestern Argentinean Low: A Study of Two Typical Events
inferredcites →https://doi.org/10.3402/tellusa.v19i2.9766openalex-snapshot
The diurnal boundary layer wind oscillation above sloping terrain1

What points at this work

Incoming claims: where this work appears in other papers’ reference lists and arguments.

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