Volume 126, Issue 20 e2021JD034541
Research Article

Upper-Tropospheric Troughs and North American Monsoon Rainfall in a Long-Term Track Dataset

Matthew R. Igel

Corresponding Author

Matthew R. Igel

Department of Land, Air and Water Resources, University of California Davis, Davis, CA, USA

Correspondence to:

M. R. Igel,

[email protected]

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Paul A. Ullrich

Paul A. Ullrich

Department of Land, Air and Water Resources, University of California Davis, Davis, CA, USA

Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA, USA

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William R. Boos

William R. Boos

Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA, USA

Department of Earth and Planetary Science, University of California Berkeley, Berkeley, CA, USA

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First published: 02 October 2021

Abstract

The North American monsoon is frequently affected by transient, propagating upper tropospheric vorticity anomalies. Sometimes called Tropical Upper-Tropospheric Troughs (TUTTs), these features have been claimed to episodically enhance monsoon rainfall. Here, we track long-lived TUTTs in 40 years of reanalysis data, producing composites and case studies from 340 TUTTs which last, on average, 7 days as they move westward across the North American monsoon region. TUTTs are thought to form from midlatitude Rossby wave breaking; case studies from our dataset support this theory. TUTTs move westward within the easterly upper-level flow in which they are embedded. In vortex-centered composites along the full tracks of long-lived TUTTs, we find no detectable increase in rainfall within the main TUTT circulation. Instead, negative precipitation anomalies lie within about 500 km of the TUTT center. Quasi-geostrophic ascent occurs in the southeast quadrant of TUTTs but is confined to the upper troposphere and does not appear to interact with precipitation. Positive anomalies of ascent and rainfall occur south and southeast of TUTTs but lie outside the main TUTT vortex, perhaps indicating concurrent variations in nearby climatological precipitation maxima. In contrast with previous case studies and subjective analyses that showed TUTTs enhance precipitation in parts of northwestern Mexico, our composites along the tracks of long-lived TUTTs portray these systems, to first order, as strong vorticity anomalies trapped in the upper troposphere that interact only weakly and indirectly with precipitation.

Key Points

  • Upper-tropospheric troughs over southwest North America are identified in an atmospheric reanalysis, yielding a 40-year track dataset

  • Tropical upper-tropospheric troughs weakly but negatively affect North American Monsoon precipitation intensity in the trough center

  • When composited along the TUTT track, enhanced precipitation falls outside the main TUTT circulation

Data Availability Statement

ERA5 data are available at https://cds.climate.copernicus.eu/#!/search?text=ERA5&type=dataset. TRMM data are available https://gpm.nasa.gov/data-access/downloads/trmm. The TempestExtremes source code is available at https://github.com/ClimateGlobalChange/tempestextremes. The new TUTT dataset is available at https://doi.org/10.25338/B8VS7T.