FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3025692854> ?p ?o ?g. }

• W3025692854 endingPage "100262" @default.
• W3025692854 startingPage "100262" @default.
• W3025692854 abstract "Abstract Extreme rainfall events in the South Pacific are widespread and affected by various factors on different time scales. We use daily rainfall data from 20 stations over the South Pacific to investigate the characteristics of extreme rainfall events from 1979 to 2018. For regional analysis, we group the stations into three clusters characterizing the western, the central, and the far eastern regions of the South Pacific Convergence Zone (SPCZ). Extreme rainfall events contribute to roughly 20% of the seasonal mean rainfall in all three clusters. Among all four factors considered, tropical cyclones (TCs) cause the highest increase in the probability (ΔpwesternSPCZ~286%, ΔpcentralSPCZ~84%, ΔpfareasternSPCZ~189%) of extreme rainfall events. The Madden-Julian Oscillation (MJO) is the second most important factor affecting the probability of extreme rainfall events, increasing it by 30–60% when the MJO is active over the western SPCZ in phases 5–6, over the central SPCZ in phases 6–7, and over the far eastern SPCZ in phases 8–1. The probability is reduced by the same order of magnitudes during the opposite dry phases of the MJO, i.e., phases 1–3 for the western and central SPCZ, and 3–6 for far the eastern SPCZ region. The probability of extreme rainfall events increases during La-Nina (El-Nino) conditions to the southwest (southeast) of the mean SPCZ by 27% (31%); however, the impact of the El-Nino and Southern Oscillation (ENSO) along the SPCZ is not apparent. Dynamical analysis shows that the favorable conditions for generating extreme rainfall events are associated with northwesterly moisture transport and its convergence. The impact of TCs, MJO, and ENSO on rainfall extreme events can be partly understood considering this dynamical analysis. Extratropical Rossby waves can trigger tropical disturbances, but their impact on extreme rainfall events is generally less important than of the TCs, MJO, and ENSO." @default.
• W3025692854 created "2020-05-21" @default.
• W3025692854 creator A5002265030 @default.
• W3025692854 creator A5052519164 @default.
• W3025692854 creator A5072464496 @default.
• W3025692854 creator A5073806842 @default.
• W3025692854 creator A5086859919 @default.
• W3025692854 creator A5087559909 @default.
• W3025692854 date "2020-09-01" @default.
• W3025692854 modified "2023-10-01" @default.
• W3025692854 title "Factors affecting extreme rainfall events in the South Pacific" @default.
• W3025692854 cites W1481976499 @default.
• W3025692854 cites W1498999946 @default.
• W3025692854 cites W1504495220 @default.
• W3025692854 cites W1512159950 @default.
• W3025692854 cites W1550927940 @default.
• W3025692854 cites W1576301207 @default.
• W3025692854 cites W1607677476 @default.
• W3025692854 cites W1645858368 @default.
• W3025692854 cites W1821734446 @default.
• W3025692854 cites W1840502663 @default.
• W3025692854 cites W1967429906 @default.
• W3025692854 cites W1972579431 @default.
• W3025692854 cites W1973673393 @default.
• W3025692854 cites W1974194630 @default.
• W3025692854 cites W1980849679 @default.
• W3025692854 cites W1984004659 @default.
• W3025692854 cites W1987971958 @default.
• W3025692854 cites W1988191164 @default.
• W3025692854 cites W1998197711 @default.
• W3025692854 cites W1998900175 @default.
• W3025692854 cites W1999125535 @default.
• W3025692854 cites W2004324197 @default.
• W3025692854 cites W2006165291 @default.
• W3025692854 cites W2016054513 @default.
• W3025692854 cites W2016160169 @default.
• W3025692854 cites W2019450357 @default.
• W3025692854 cites W2022548072 @default.
• W3025692854 cites W2025453528 @default.
• W3025692854 cites W2025529786 @default.
• W3025692854 cites W2026630001 @default.
• W3025692854 cites W2029009181 @default.
• W3025692854 cites W2030871959 @default.
• W3025692854 cites W2033175940 @default.
• W3025692854 cites W2033553637 @default.
• W3025692854 cites W2036366698 @default.
• W3025692854 cites W2046853662 @default.
• W3025692854 cites W2048679312 @default.
• W3025692854 cites W2050414673 @default.
• W3025692854 cites W2052269429 @default.
• W3025692854 cites W2054655850 @default.
• W3025692854 cites W2056867457 @default.
• W3025692854 cites W2058798762 @default.
• W3025692854 cites W2065159862 @default.
• W3025692854 cites W2068491339 @default.
• W3025692854 cites W2071949631 @default.
• W3025692854 cites W2088055301 @default.
• W3025692854 cites W2092497323 @default.
• W3025692854 cites W2096538718 @default.
• W3025692854 cites W2100593605 @default.
• W3025692854 cites W2108038169 @default.
• W3025692854 cites W2108436816 @default.
• W3025692854 cites W2110365135 @default.
• W3025692854 cites W2110635517 @default.
• W3025692854 cites W2111281446 @default.
• W3025692854 cites W2113435709 @default.
• W3025692854 cites W2118544834 @default.
• W3025692854 cites W2120618726 @default.
• W3025692854 cites W2121745948 @default.
• W3025692854 cites W2122936763 @default.
• W3025692854 cites W2124020917 @default.
• W3025692854 cites W2124971768 @default.
• W3025692854 cites W2130654208 @default.
• W3025692854 cites W2136321541 @default.
• W3025692854 cites W2139396291 @default.
• W3025692854 cites W2148459731 @default.
• W3025692854 cites W2160979277 @default.
• W3025692854 cites W2163932246 @default.
• W3025692854 cites W2164136606 @default.
• W3025692854 cites W2167221624 @default.
• W3025692854 cites W2167622596 @default.
• W3025692854 cites W2168330718 @default.
• W3025692854 cites W2172827512 @default.
• W3025692854 cites W2173519424 @default.
• W3025692854 cites W2174485535 @default.
• W3025692854 cites W2176050019 @default.
• W3025692854 cites W2176774719 @default.
• W3025692854 cites W2176967258 @default.
• W3025692854 cites W2194618511 @default.
• W3025692854 cites W2238606243 @default.
• W3025692854 cites W2255656880 @default.
• W3025692854 cites W2527976556 @default.
• W3025692854 cites W2581074662 @default.
• W3025692854 cites W2590361842 @default.
• W3025692854 cites W2750737179 @default.
• W3025692854 cites W2757937750 @default.
• W3025692854 cites W2951813082 @default.
• W3025692854 cites W2952178951 @default.

• next