Annual Modulation of Diurnal Winds in the Tropical Oceans

Projections of future climate are sensitive to the representation of upper-ocean diurnal variability, including the diurnal cycle of winds. Two different methods suitable for time series with missing data are used here to characterize how observed diurnal winds vary over the year. One is based on di...

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Main Authors: Donata Giglio, Sarah T. Gille, Bruce D. Cornuelle, Aneesh C. Subramanian, F. Joseph Turk, Svetla Hristova-Veleva, Devon Northcott
Format: Article
Language:English
Published: MDPI AG 2022-01-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/14/3/459
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author Donata Giglio
Sarah T. Gille
Bruce D. Cornuelle
Aneesh C. Subramanian
F. Joseph Turk
Svetla Hristova-Veleva
Devon Northcott
author_facet Donata Giglio
Sarah T. Gille
Bruce D. Cornuelle
Aneesh C. Subramanian
F. Joseph Turk
Svetla Hristova-Veleva
Devon Northcott
author_sort Donata Giglio
collection DOAJ
description Projections of future climate are sensitive to the representation of upper-ocean diurnal variability, including the diurnal cycle of winds. Two different methods suitable for time series with missing data are used here to characterize how observed diurnal winds vary over the year. One is based on diurnal composites of mooring data, and the other is based on harmonic analysis via a least squares fit and is able to isolate annual (i.e., 1 cycle per year) modulation of diurnal variability. Results show that the diurnal amplitude in meridional winds is larger than in zonal winds and peaks in the tropical Pacific, where diurnal variability in zonal winds is overall weaker compared to other basins. Furthermore, the amplitude and phasing of diurnal winds in the tropical oceans are not uniform in time, with overall larger differences through the year in the meridional component of tropical winds. Estimating the annual modulation of the diurnal signal implies resolving both the diurnal energy peak and also the modulation of this peak by the annual cycle. This leads to a recommendation for sampling at least 6 times per day and for a duration of at least 3 years.
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spelling doaj.art-79e4d53aa44243cfa15622db9a355bb82023-11-23T17:38:00ZengMDPI AGRemote Sensing2072-42922022-01-0114345910.3390/rs14030459Annual Modulation of Diurnal Winds in the Tropical OceansDonata Giglio0Sarah T. Gille1Bruce D. Cornuelle2Aneesh C. Subramanian3F. Joseph Turk4Svetla Hristova-Veleva5Devon Northcott6Department of Atmospheric and Oceanic Sciences, University of Colorado Boulder, Boulder, CO 80309, USAScripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92093, USAScripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92093, USADepartment of Atmospheric and Oceanic Sciences, University of Colorado Boulder, Boulder, CO 80309, USAJet Propulsion Laboratory (JPL), California Institute of Technology, Pasadena, CA 91109, USAJet Propulsion Laboratory (JPL), California Institute of Technology, Pasadena, CA 91109, USAScripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92093, USAProjections of future climate are sensitive to the representation of upper-ocean diurnal variability, including the diurnal cycle of winds. Two different methods suitable for time series with missing data are used here to characterize how observed diurnal winds vary over the year. One is based on diurnal composites of mooring data, and the other is based on harmonic analysis via a least squares fit and is able to isolate annual (i.e., 1 cycle per year) modulation of diurnal variability. Results show that the diurnal amplitude in meridional winds is larger than in zonal winds and peaks in the tropical Pacific, where diurnal variability in zonal winds is overall weaker compared to other basins. Furthermore, the amplitude and phasing of diurnal winds in the tropical oceans are not uniform in time, with overall larger differences through the year in the meridional component of tropical winds. Estimating the annual modulation of the diurnal signal implies resolving both the diurnal energy peak and also the modulation of this peak by the annual cycle. This leads to a recommendation for sampling at least 6 times per day and for a duration of at least 3 years.https://www.mdpi.com/2072-4292/14/3/459tropical windsdiurnal variabilityannual modulation
spellingShingle Donata Giglio
Sarah T. Gille
Bruce D. Cornuelle
Aneesh C. Subramanian
F. Joseph Turk
Svetla Hristova-Veleva
Devon Northcott
Annual Modulation of Diurnal Winds in the Tropical Oceans
Remote Sensing
tropical winds
diurnal variability
annual modulation
title Annual Modulation of Diurnal Winds in the Tropical Oceans
title_full Annual Modulation of Diurnal Winds in the Tropical Oceans
title_fullStr Annual Modulation of Diurnal Winds in the Tropical Oceans
title_full_unstemmed Annual Modulation of Diurnal Winds in the Tropical Oceans
title_short Annual Modulation of Diurnal Winds in the Tropical Oceans
title_sort annual modulation of diurnal winds in the tropical oceans
topic tropical winds
diurnal variability
annual modulation
url https://www.mdpi.com/2072-4292/14/3/459
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