Interannual variability in associations between seasonal climate, weather, and extremes
Wintertime temperature over the Southwestern United States
Bibliographic Data
| ID | 15548768 |
|---|---|
| Authors | Kristen Guirguis (0000-0002-5274-0225, Scripps Institution of Oceanography, corresponding author), Alexander Gershunov (0000-0002-6598-6638, Scripps Institution of Oceanography), Daniel R Cayan (0000-0002-2719-6811, Scripps Institution of Oceanography) |
| Year | 2015 |
| Volume | 10 |
| Issue | 12 |
| Pages | 124023-124023 |
| Publication date | 2015-12-01 |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Environmental Research Letters (JOURNAL) |
| Journal identifiers | ISSN: 1748-9326 • E-ISSN: 1748-9326 |
| Publisher | IOP Publishing (PUBLISHER • GB) |
| DOI | 10.1088/1748-9326/10/12/124023 |
| OpenAlex | W2255988337 |
| Language | EN |
| Citations received | 1 |
| References cited | 16 |
Temperature variability in the Southwest US is investigated using skew-normal probability distribution functions (SN PDFs) fitted to observed wintertime daily maximum temperature records. These PDFs vary significantly between years, with important geographical differences in the relationship between the central tendency and tails, revealing differing linkages between weather and climate. The warmest and coldest extremes do not necessarily follow the distribution center. In some regions one tail of the distribution shows more variability than does the other. For example, in California the cold tail is more variable while the warm tail remains relatively stable, so warm years are associated with fewer cold extremes but not necessarily more warm extremes. The opposite relationship is seen in the Great Plains. Changes in temperature PDFs are conditioned by different phases of El Nio-La Nia (ENSO) and the Pacific decadal oscillation (PDO). In the Southern Great Plains, La Nia and/or negative PDO are associated with generally warmer conditions. However, in terms of extremes, while the warm tails become thicker and longer, the cool tails are not impactedextremely warm days become more frequent but extremely cool days are not less frequent. In contrast, in coastal California, La Nia or negative PDO bring generally cooler conditions with more/stronger cold extremes but the warm extreme probability is not significantly affected. These results could have implications for global warming. If a rigid shift of the whole range occurs, then warm years are not necessarily a good analogue for a warmer climate. If global warming instead brings regional changes more aligned with a preferred state of dominant climate variability modes, then we may see asymmetric changes in the tails of local temperature PDFs
Atmospheric sciences · Climate change · Climate extremes · Climatology · Global warming · Range (aeronautics · Climate variability and models · Environmental Science · Hydrology and Drought Analysis · Meteorological Phenomena and Simulations · Geology · Oceanography
| Citations per year | 0.33 |
|---|---|
| Citation span | 2023 - 2023 (1) |
| Highly cited | No |