Student Hands-on Atmospheric Discovery during an Eclipse (SHADE) Over Texas

Audrey Garza Texas A&M University-Corpus Christi

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Chuntao Liu Texas A&M University-Corpus Christi

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Thomas Lavigne Texas A&M University-Corpus Christi

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Florian Morvais Texas A&M University-Corpus Christi

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Quincy Walker Texas A&M University-Corpus Christi

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Hailey Santa Ana Texas A&M University-Corpus Christi

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Jerricca Rossilli Texas A&M University-Corpus Christi

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Delaynie Peters Texas A&M University-Corpus Christi

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Carl Meade Texas A&M University-Corpus Christi

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Juan Camacho Texas A&M University-Corpus Christi

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Paul Walter St. Edward’s University

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Abstract

On 8 April 2024, a total solar eclipse overpassed Texas in the southern portion of the United States. To monitor the impact of the total solar eclipse, a group of students from Texas A&M University-Corpus Christi developed two weather balloon payloads and six ground-based instrument packages using microcontrollers and low-cost sensors. These instrument packages were deployed to six different sites spanning nearly 600 km along the total eclipse path from the Mexican border to North Texas. During the total eclipse, air temperature decreased, and relative humidity increased consistently at all six stations due to the reduction of sensible heating. The dew point temperatures decreased at the near surface at all sites likely due to the reduction of evaporation. Five of the six ground stations observed a slight dampening of the windspeed, two of the six stations recorded significant counterclockwise wind shifts. No consistent pattern was observed in the surface vertical electric field at the six ground stations. The two balloon payloads captured the damping of the visible and ultraviolet (UV) radiation in the upper troposphere and lower stratosphere throughout the event. Though a slight decrease in both temperature and ozone in the lower stratosphere were observed after the totality, it is difficult to determine the impact from the eclipse on the ozone mixing ratio and dynamics in the lower stratosphere from only a few vertical profiles. For the students who participated, this field campaign has provided invaluable experiences in instrumentation, field work, and data collection.

© 2025 American Meteorological Society. This is an Author Accepted Manuscript distributed under the terms of the default AMS reuse license. For information regarding reuse and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/PUBSReuseLicenses).

Corresponding Author: Audrey Garza, Department of Atmospheric Sciences, Texas A&M University-Corpus Christi, 6300 Ocean Dr., Corpus Christi, 78412-5858. email: audrey.garza1@tamucc.edu

Abstract

On 8 April 2024, a total solar eclipse overpassed Texas in the southern portion of the United States. To monitor the impact of the total solar eclipse, a group of students from Texas A&M University-Corpus Christi developed two weather balloon payloads and six ground-based instrument packages using microcontrollers and low-cost sensors. These instrument packages were deployed to six different sites spanning nearly 600 km along the total eclipse path from the Mexican border to North Texas. During the total eclipse, air temperature decreased, and relative humidity increased consistently at all six stations due to the reduction of sensible heating. The dew point temperatures decreased at the near surface at all sites likely due to the reduction of evaporation. Five of the six ground stations observed a slight dampening of the windspeed, two of the six stations recorded significant counterclockwise wind shifts. No consistent pattern was observed in the surface vertical electric field at the six ground stations. The two balloon payloads captured the damping of the visible and ultraviolet (UV) radiation in the upper troposphere and lower stratosphere throughout the event. Though a slight decrease in both temperature and ozone in the lower stratosphere were observed after the totality, it is difficult to determine the impact from the eclipse on the ozone mixing ratio and dynamics in the lower stratosphere from only a few vertical profiles. For the students who participated, this field campaign has provided invaluable experiences in instrumentation, field work, and data collection.

© 2025 American Meteorological Society. This is an Author Accepted Manuscript distributed under the terms of the default AMS reuse license. For information regarding reuse and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/PUBSReuseLicenses).

Corresponding Author: Audrey Garza, Department of Atmospheric Sciences, Texas A&M University-Corpus Christi, 6300 Ocean Dr., Corpus Christi, 78412-5858. email: audrey.garza1@tamucc.edu
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