Hunting for gravity waves in non-orographic winter storms using 3+ years of regional surface air pressure network and radar observations
<p>Atmospheric gravity waves (i.e., buoyancy waves) can occur within stable layers when vertical oscillations are triggered by localized heating, flow over terrain, or imbalances in upper-level flow. Case studies of winter storms have associated gravity waves with heavier surface snowfall accu...
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Copernicus Publications
2025-02-01
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| Series: | Atmospheric Chemistry and Physics |
| Online Access: | https://acp.copernicus.org/articles/25/1765/2025/acp-25-1765-2025.pdf |
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| author | L. R. Allen L. R. Allen S. E. Yuter S. E. Yuter M. A. Miller L. M. Tomkins L. M. Tomkins |
| author_facet | L. R. Allen L. R. Allen S. E. Yuter S. E. Yuter M. A. Miller L. M. Tomkins L. M. Tomkins |
| author_sort | L. R. Allen |
| collection | DOAJ |
| description | <p>Atmospheric gravity waves (i.e., buoyancy waves) can occur within stable layers when vertical oscillations are triggered by localized heating, flow over terrain, or imbalances in upper-level flow. Case studies of winter storms have associated gravity waves with heavier surface snowfall accumulations, but the representativeness of those findings for settings without orographic precipitation has not been previously addressed.</p>
<p>We deployed networks of high-precision pressure sensors from January 2020 to April 2023 in and around Toronto, ON, Canada, and New York, NY, USA, two regions without strong topographic forcing. Pressure wave events were identified when at least four sensors in a network detected propagating pressure waves with wave periods <span class="inline-formula">≤67</span> <span class="inline-formula">min</span>, wavelengths <span class="inline-formula">≤170</span> <span class="inline-formula">km</span>, and amplitudes <span class="inline-formula">≥0.45</span> <span class="inline-formula">hPa</span>. Reanalysis model output and operational weather observations provided environmental context for each gravity wave event. We detected 33 pressure wave events across 40 months of data; of these events, 23 were gravity waves, whereas the rest were frontal passages, outflow boundary passages, or a wake low. We found a strong linear relationship between amplitude and event duration for the 23 atmospheric gravity wave events.</p>
<p>Gravity wave events are rare in non-orographic snow storms in our study region. Of the 594 h with <span class="inline-formula">≥0.1</span> <span class="inline-formula">mm h<sup>−1</sup></span> (liquid equivalent) of snow sampled, only 19 h was during a gravity wave event. When gravity waves and enhanced reflectivity bands within snow co-occurred, the bands did not move in a direction or at a velocity consistent with the pressure waves. In agreement with previous work, most of our gravity wave events are associated with strong upper-level flow imbalances to the south or west of their location.</p> |
| format | Article |
| id | doaj-art-d8c0f2accf574b7dabb6b392bb0ca85a |
| institution | Kabale University |
| issn | 1680-7316 1680-7324 |
| language | English |
| publishDate | 2025-02-01 |
| publisher | Copernicus Publications |
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| series | Atmospheric Chemistry and Physics |
| spelling | doaj-art-d8c0f2accf574b7dabb6b392bb0ca85a2025-02-07T10:50:28ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242025-02-01251765179010.5194/acp-25-1765-2025Hunting for gravity waves in non-orographic winter storms using 3+ years of regional surface air pressure network and radar observationsL. R. Allen0L. R. Allen1S. E. Yuter2S. E. Yuter3M. A. Miller4L. M. Tomkins5L. M. Tomkins6Center for Geospatial Analytics, North Carolina State University, Raleigh, NC 27695, USAcurrent address: Department of Meteorology, Stockholm University, 10691 Stockholm, SwedenCenter for Geospatial Analytics, North Carolina State University, Raleigh, NC 27695, USADepartment of Marine, Earth, and Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695, USADepartment of Marine, Earth, and Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695, USACenter for Geospatial Analytics, North Carolina State University, Raleigh, NC 27695, USAcurrent address: Karen Clark and Company, Boston, MA 02116, USA<p>Atmospheric gravity waves (i.e., buoyancy waves) can occur within stable layers when vertical oscillations are triggered by localized heating, flow over terrain, or imbalances in upper-level flow. Case studies of winter storms have associated gravity waves with heavier surface snowfall accumulations, but the representativeness of those findings for settings without orographic precipitation has not been previously addressed.</p> <p>We deployed networks of high-precision pressure sensors from January 2020 to April 2023 in and around Toronto, ON, Canada, and New York, NY, USA, two regions without strong topographic forcing. Pressure wave events were identified when at least four sensors in a network detected propagating pressure waves with wave periods <span class="inline-formula">≤67</span> <span class="inline-formula">min</span>, wavelengths <span class="inline-formula">≤170</span> <span class="inline-formula">km</span>, and amplitudes <span class="inline-formula">≥0.45</span> <span class="inline-formula">hPa</span>. Reanalysis model output and operational weather observations provided environmental context for each gravity wave event. We detected 33 pressure wave events across 40 months of data; of these events, 23 were gravity waves, whereas the rest were frontal passages, outflow boundary passages, or a wake low. We found a strong linear relationship between amplitude and event duration for the 23 atmospheric gravity wave events.</p> <p>Gravity wave events are rare in non-orographic snow storms in our study region. Of the 594 h with <span class="inline-formula">≥0.1</span> <span class="inline-formula">mm h<sup>−1</sup></span> (liquid equivalent) of snow sampled, only 19 h was during a gravity wave event. When gravity waves and enhanced reflectivity bands within snow co-occurred, the bands did not move in a direction or at a velocity consistent with the pressure waves. In agreement with previous work, most of our gravity wave events are associated with strong upper-level flow imbalances to the south or west of their location.</p>https://acp.copernicus.org/articles/25/1765/2025/acp-25-1765-2025.pdf |
| spellingShingle | L. R. Allen L. R. Allen S. E. Yuter S. E. Yuter M. A. Miller L. M. Tomkins L. M. Tomkins Hunting for gravity waves in non-orographic winter storms using 3+ years of regional surface air pressure network and radar observations Atmospheric Chemistry and Physics |
| title | Hunting for gravity waves in non-orographic winter storms using 3+ years of regional surface air pressure network and radar observations |
| title_full | Hunting for gravity waves in non-orographic winter storms using 3+ years of regional surface air pressure network and radar observations |
| title_fullStr | Hunting for gravity waves in non-orographic winter storms using 3+ years of regional surface air pressure network and radar observations |
| title_full_unstemmed | Hunting for gravity waves in non-orographic winter storms using 3+ years of regional surface air pressure network and radar observations |
| title_short | Hunting for gravity waves in non-orographic winter storms using 3+ years of regional surface air pressure network and radar observations |
| title_sort | hunting for gravity waves in non orographic winter storms using 3 years of regional surface air pressure network and radar observations |
| url | https://acp.copernicus.org/articles/25/1765/2025/acp-25-1765-2025.pdf |
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