Hydrological cycle changes explain weak snowball earth storm track despite increased surface baroclinicity
Simulations show that storm tracks were weaker during past cold, icy climates relative to the modern climate despite increased surface baroclinicity. Previous work explained the weak North Atlantic storm track during the Last Glacial Maximum using dry zonally asymmetric mechanisms associated with or...
| Những tác giả chính: | , |
|---|---|
| Định dạng: | Journal article |
| Ngôn ngữ: | English |
| Được phát hành: |
Wiley
2020
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| _version_ | 1826272212586332160 |
|---|---|
| author | Shaw, TA Graham, RJ |
| author_facet | Shaw, TA Graham, RJ |
| author_sort | Shaw, TA |
| collection | OXFORD |
| description | Simulations show that storm tracks were weaker during past cold, icy climates relative to the modern climate despite increased surface baroclinicity. Previous work explained the weak North Atlantic storm track during the Last Glacial Maximum using dry zonally asymmetric mechanisms associated with orographic forcing. Here we show that zonally symmetric mechanisms associated with the hydrological cycle explain the weak Snowball Earth storm track. The weak storm track is consistent with the decreased meridional gradient of evaporation and atmospheric shortwave absorption and can be predicted following global mean cooling and the Clausius-Clapeyron relation. The weak storm track is also consistent with decreased latent heat release aloft in the tropics, which decreases upper tropospheric baroclinicity and mean available potential energy. Overall, both hydrological cycle mechanisms are reflected in the significant correlation between storm track intensity and the meridional surface moist static energy gradient across a range of simulated climates between modern and Snowball Earth. |
| first_indexed | 2024-03-06T22:08:58Z |
| format | Journal article |
| id | oxford-uuid:51234d36-f73b-4d10-b4ce-d29b9f9eb7fa |
| institution | University of Oxford |
| language | English |
| last_indexed | 2024-03-06T22:08:58Z |
| publishDate | 2020 |
| publisher | Wiley |
| record_format | dspace |
| spelling | oxford-uuid:51234d36-f73b-4d10-b4ce-d29b9f9eb7fa2022-03-26T16:17:41ZHydrological cycle changes explain weak snowball earth storm track despite increased surface baroclinicity Journal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:51234d36-f73b-4d10-b4ce-d29b9f9eb7faEnglishSymplectic ElementsWiley2020Shaw, TAGraham, RJSimulations show that storm tracks were weaker during past cold, icy climates relative to the modern climate despite increased surface baroclinicity. Previous work explained the weak North Atlantic storm track during the Last Glacial Maximum using dry zonally asymmetric mechanisms associated with orographic forcing. Here we show that zonally symmetric mechanisms associated with the hydrological cycle explain the weak Snowball Earth storm track. The weak storm track is consistent with the decreased meridional gradient of evaporation and atmospheric shortwave absorption and can be predicted following global mean cooling and the Clausius-Clapeyron relation. The weak storm track is also consistent with decreased latent heat release aloft in the tropics, which decreases upper tropospheric baroclinicity and mean available potential energy. Overall, both hydrological cycle mechanisms are reflected in the significant correlation between storm track intensity and the meridional surface moist static energy gradient across a range of simulated climates between modern and Snowball Earth. |
| spellingShingle | Shaw, TA Graham, RJ Hydrological cycle changes explain weak snowball earth storm track despite increased surface baroclinicity |
| title | Hydrological cycle changes explain weak snowball earth storm track despite increased surface baroclinicity |
| title_full | Hydrological cycle changes explain weak snowball earth storm track despite increased surface baroclinicity |
| title_fullStr | Hydrological cycle changes explain weak snowball earth storm track despite increased surface baroclinicity |
| title_full_unstemmed | Hydrological cycle changes explain weak snowball earth storm track despite increased surface baroclinicity |
| title_short | Hydrological cycle changes explain weak snowball earth storm track despite increased surface baroclinicity |
| title_sort | hydrological cycle changes explain weak snowball earth storm track despite increased surface baroclinicity |
| work_keys_str_mv | AT shawta hydrologicalcyclechangesexplainweaksnowballearthstormtrackdespiteincreasedsurfacebaroclinicity AT grahamrj hydrologicalcyclechangesexplainweaksnowballearthstormtrackdespiteincreasedsurfacebaroclinicity |