Matches in SemOpenAlex for { <https://semopenalex.org/work/W3181445727> ?p ?o ?g. }
- W3181445727 endingPage "103557" @default.
- W3181445727 startingPage "103557" @default.
- W3181445727 abstract "The mid-Pliocene warm period (~3.3–3 million years ago) sustained similar atmospheric CO2 concentrations to today, and is thus considered one of the best recent paleoclimate analogs for a future warmer climate. Using model simulations following the Pliocene Model Intercomparison Project Phase 2 experimental design, we investigate the mid-Pliocene mid-latitude hydroclimate with a focus on Pacific atmospheric rivers and related changes to mean and extreme precipitation over the Americas. We find distinct spatial patterns of change in precipitation compared to the pre-industrial control simulation in the northern and southern hemispheres; specifically, the Pacific coasts of North America and Chile, two regions where atmospheric rivers strongly influence local weather and climate today, experience opposite signs of change in precipitation. The precipitation changes are linked to dynamical shifts in atmospheric rivers, especially in the Northern Hemisphere. There, a wintertime stationary wave train present in the pre-industrial control nearly disappears in the mid-Pliocene simulation, resulting in fewer atmospheric rivers making landfall over western North America. Sensitivity simulations reveal that model boundary conditions for mid-Pliocene ice sheets and topography, applied in isolation or in combination, cause the relevant stationary wave response independently of CO2 forcing. The stationary wave response to surface boundary conditions weakens the analogy between mid-Pliocene and future regional midlatitude hydroclimate, and informs our interpretation of the apparent discrepancy between modeled precipitation and hydroclimate proxies in western North America." @default.
- W3181445727 created "2021-07-19" @default.
- W3181445727 creator A5003913110 @default.
- W3181445727 creator A5062577480 @default.
- W3181445727 creator A5077809116 @default.
- W3181445727 creator A5083723512 @default.
- W3181445727 date "2021-09-01" @default.
- W3181445727 modified "2023-09-30" @default.
- W3181445727 title "Influence of stationary waves on mid-Pliocene atmospheric rivers and hydroclimate" @default.
- W3181445727 cites W1489614333 @default.
- W3181445727 cites W1669944625 @default.
- W3181445727 cites W1733916393 @default.
- W3181445727 cites W1964913251 @default.
- W3181445727 cites W1968176769 @default.
- W3181445727 cites W1969308283 @default.
- W3181445727 cites W1978656522 @default.
- W3181445727 cites W1979082953 @default.
- W3181445727 cites W1979722804 @default.
- W3181445727 cites W1983146950 @default.
- W3181445727 cites W1985217958 @default.
- W3181445727 cites W1991021495 @default.
- W3181445727 cites W1993112115 @default.
- W3181445727 cites W1999778821 @default.
- W3181445727 cites W2000057625 @default.
- W3181445727 cites W2001575273 @default.
- W3181445727 cites W2004451060 @default.
- W3181445727 cites W2006547330 @default.
- W3181445727 cites W2007489277 @default.
- W3181445727 cites W2010035565 @default.
- W3181445727 cites W2023188259 @default.
- W3181445727 cites W2024922828 @default.
- W3181445727 cites W2033098709 @default.
- W3181445727 cites W2037106791 @default.
- W3181445727 cites W2042092867 @default.
- W3181445727 cites W2044904655 @default.
- W3181445727 cites W2052734296 @default.
- W3181445727 cites W2058068642 @default.
- W3181445727 cites W2059517603 @default.
- W3181445727 cites W2060135956 @default.
- W3181445727 cites W2061328952 @default.
- W3181445727 cites W2067310122 @default.
- W3181445727 cites W2069620066 @default.
- W3181445727 cites W2069812110 @default.
- W3181445727 cites W2074250709 @default.
- W3181445727 cites W2083367302 @default.
- W3181445727 cites W2090354893 @default.
- W3181445727 cites W2090467588 @default.
- W3181445727 cites W2093401535 @default.
- W3181445727 cites W2096425009 @default.
- W3181445727 cites W2096760370 @default.
- W3181445727 cites W2098193783 @default.
- W3181445727 cites W2098278536 @default.
- W3181445727 cites W2106929434 @default.
- W3181445727 cites W2113803029 @default.
- W3181445727 cites W2118061256 @default.
- W3181445727 cites W2120618726 @default.
- W3181445727 cites W2122511023 @default.
- W3181445727 cites W2124783839 @default.
- W3181445727 cites W2125290109 @default.
- W3181445727 cites W2127070782 @default.
- W3181445727 cites W2129831404 @default.
- W3181445727 cites W2132276806 @default.
- W3181445727 cites W2135648148 @default.
- W3181445727 cites W2137966020 @default.
- W3181445727 cites W2138644576 @default.
- W3181445727 cites W2141442289 @default.
- W3181445727 cites W2146062664 @default.
- W3181445727 cites W2146200079 @default.
- W3181445727 cites W2149177797 @default.
- W3181445727 cites W2152578450 @default.
- W3181445727 cites W2152928439 @default.
- W3181445727 cites W2160430092 @default.
- W3181445727 cites W2161251360 @default.
- W3181445727 cites W2162215191 @default.
- W3181445727 cites W2164094029 @default.
- W3181445727 cites W2172782380 @default.
- W3181445727 cites W2174421778 @default.
- W3181445727 cites W2174892202 @default.
- W3181445727 cites W2180956791 @default.
- W3181445727 cites W2189851893 @default.
- W3181445727 cites W2270241547 @default.
- W3181445727 cites W2274616641 @default.
- W3181445727 cites W2294682052 @default.
- W3181445727 cites W2302375105 @default.
- W3181445727 cites W2302862193 @default.
- W3181445727 cites W2306905182 @default.
- W3181445727 cites W2316378793 @default.
- W3181445727 cites W2320306031 @default.
- W3181445727 cites W2325260652 @default.
- W3181445727 cites W2328573691 @default.
- W3181445727 cites W2345906900 @default.
- W3181445727 cites W2475938390 @default.
- W3181445727 cites W2512447799 @default.
- W3181445727 cites W2551200285 @default.
- W3181445727 cites W2600489599 @default.
- W3181445727 cites W2616273741 @default.
- W3181445727 cites W2729353881 @default.
- W3181445727 cites W2739350628 @default.