Recent Changes in Mid-latitude Wave Propagation
In recent years climate change in the polar areas has attracted a lot of attention. Not only for its consequences in polar areas, but also for its possible effects on lower latitudes. A reduced temperature gradient between the polar areas is expected to weaken the mid-latitude jet stream. This weake...
Main Author: | |
---|---|
Format: | Master Thesis |
Language: | English |
Published: |
UiT Norges arktiske universitet
2024
|
Subjects: | |
Online Access: | https://hdl.handle.net/10037/34027 |
_version_ | 1829299119804383232 |
---|---|
author | Attema, Ronnie |
author_facet | Attema, Ronnie |
author_sort | Attema, Ronnie |
collection | University of Tromsø: Munin Open Research Archive |
description | In recent years climate change in the polar areas has attracted a lot of attention. Not only for its consequences in polar areas, but also for its possible effects on lower latitudes. A reduced temperature gradient between the polar areas is expected to weaken the mid-latitude jet stream. This weaker jet stream is hypothesised to lead to a reduction in the propagation velocity of atmospheric Rossby waves and lead to more persistent weather. In this study we will investigate these changes in wave propagation by computing the wave activity and wave activity flux from the ERA5 reanalysis for the time period 1990- 2020. We find that there are significant changes in the wave activity and wave activity flux, but not in the wave forcing of the mean flow. We find a seasonal and geographic dependency for the trends in the wave activity and its flux. We furthermore provide evidence that these changes can be linked to low sea ice concentrations. In addition we explore the relationship between the wave activity and the temperature. For this we find that a high wave-activity in general results in a negative temperature anomaly, but during the winter a high wave-activity is related to a positive temperature anomaly for some areas. |
format | Master Thesis |
genre | Sea ice |
genre_facet | Sea ice |
id | ftunivtroemsoe:oai:munin.uit.no:10037/34027 |
institution | Open Polar |
language | English |
op_collection_id | ftunivtroemsoe |
op_relation | https://hdl.handle.net/10037/34027 |
op_rights | Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) Copyright 2024 The Author(s) https://creativecommons.org/licenses/by-nc-sa/4.0 |
publishDate | 2024 |
publisher | UiT Norges arktiske universitet |
record_format | openpolar |
spelling | ftunivtroemsoe:oai:munin.uit.no:10037/34027 2025-04-13T14:26:51+00:00 Recent Changes in Mid-latitude Wave Propagation Attema, Ronnie 2024-06-12 https://hdl.handle.net/10037/34027 eng eng UiT Norges arktiske universitet UiT The Arctic University of Norway https://hdl.handle.net/10037/34027 Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) Copyright 2024 The Author(s) https://creativecommons.org/licenses/by-nc-sa/4.0 atmospheric physics physics rossby waves wave activity wave activity flux FYS-3900 Mastergradsoppgave Master thesis 2024 ftunivtroemsoe 2025-03-14T05:17:57Z In recent years climate change in the polar areas has attracted a lot of attention. Not only for its consequences in polar areas, but also for its possible effects on lower latitudes. A reduced temperature gradient between the polar areas is expected to weaken the mid-latitude jet stream. This weaker jet stream is hypothesised to lead to a reduction in the propagation velocity of atmospheric Rossby waves and lead to more persistent weather. In this study we will investigate these changes in wave propagation by computing the wave activity and wave activity flux from the ERA5 reanalysis for the time period 1990- 2020. We find that there are significant changes in the wave activity and wave activity flux, but not in the wave forcing of the mean flow. We find a seasonal and geographic dependency for the trends in the wave activity and its flux. We furthermore provide evidence that these changes can be linked to low sea ice concentrations. In addition we explore the relationship between the wave activity and the temperature. For this we find that a high wave-activity in general results in a negative temperature anomaly, but during the winter a high wave-activity is related to a positive temperature anomaly for some areas. Master Thesis Sea ice University of Tromsø: Munin Open Research Archive |
spellingShingle | atmospheric physics physics rossby waves wave activity wave activity flux FYS-3900 Attema, Ronnie Recent Changes in Mid-latitude Wave Propagation |
title | Recent Changes in Mid-latitude Wave Propagation |
title_full | Recent Changes in Mid-latitude Wave Propagation |
title_fullStr | Recent Changes in Mid-latitude Wave Propagation |
title_full_unstemmed | Recent Changes in Mid-latitude Wave Propagation |
title_short | Recent Changes in Mid-latitude Wave Propagation |
title_sort | recent changes in mid-latitude wave propagation |
topic | atmospheric physics physics rossby waves wave activity wave activity flux FYS-3900 |
topic_facet | atmospheric physics physics rossby waves wave activity wave activity flux FYS-3900 |
url | https://hdl.handle.net/10037/34027 |