Matches in SemOpenAlex for { <https://semopenalex.org/work/W2890693518> ?p ?o ?g. }
- W2890693518 endingPage "245" @default.
- W2890693518 startingPage "234" @default.
- W2890693518 abstract "Abstract Understanding the magnitude, timing and drivers of regional variations in paleotemperature is often challenging because of the lack of a similar proxy in every climate zone and differences in the temperature-proxy response relationship of the multiple proxies across large spatial scales. Borehole temperature data show promise for elucidating regional variation of paleotemperature because of their applicability in all climate zones. We reconstructed surface temperature histories for the past 2000 years, using borehole temperature data from four study regions within eastern Australia. Borehole temperatures across all four areas show warming since the 19th Century with most rapid warming occurring during the 20th Century. Reconstructions reveal significant spatial and temporal variation of paleotemperature between each region, with the south-east coast of the Australian mainland (Victoria) being the most different. Here, temperatures display a Little Ice Age (LIA) type response, decreasing during the 16th to 18th Century with a peak cold temperature of −0.6 °C during 1700 CE relative to the long term average spanning 0 to 1000 CE where temperature changes are negligible. Further, comparison with proxy data suggests temperature increases affected moisture balances in tropical and temperate regions differently. In the northern tropics, increased temperatures correlated with wetter conditions, while in the southern, more Mediterranean climate regions, warmer periods were generally drier." @default.
- W2890693518 created "2018-09-27" @default.
- W2890693518 creator A5037795633 @default.
- W2890693518 creator A5047840078 @default.
- W2890693518 creator A5053468073 @default.
- W2890693518 date "2018-11-01" @default.
- W2890693518 modified "2023-09-23" @default.
- W2890693518 title "Eastern Australian late Holocene paleotemperature variation inferred from borehole temperature data" @default.
- W2890693518 cites W1609047602 @default.
- W2890693518 cites W1660201747 @default.
- W2890693518 cites W1887481902 @default.
- W2890693518 cites W1965014451 @default.
- W2890693518 cites W1966682789 @default.
- W2890693518 cites W1969160941 @default.
- W2890693518 cites W1972868553 @default.
- W2890693518 cites W1974470230 @default.
- W2890693518 cites W1977309379 @default.
- W2890693518 cites W1978291154 @default.
- W2890693518 cites W1980948514 @default.
- W2890693518 cites W1982630646 @default.
- W2890693518 cites W1983199477 @default.
- W2890693518 cites W1985142385 @default.
- W2890693518 cites W1985282519 @default.
- W2890693518 cites W1989182850 @default.
- W2890693518 cites W1995636178 @default.
- W2890693518 cites W1997133968 @default.
- W2890693518 cites W2002988376 @default.
- W2890693518 cites W2005686580 @default.
- W2890693518 cites W2007012175 @default.
- W2890693518 cites W2008932119 @default.
- W2890693518 cites W2008967194 @default.
- W2890693518 cites W2013641113 @default.
- W2890693518 cites W2014363923 @default.
- W2890693518 cites W2014602425 @default.
- W2890693518 cites W2014968686 @default.
- W2890693518 cites W2015703005 @default.
- W2890693518 cites W2017973926 @default.
- W2890693518 cites W2018389746 @default.
- W2890693518 cites W2019819269 @default.
- W2890693518 cites W2019924778 @default.
- W2890693518 cites W2021606434 @default.
- W2890693518 cites W2021612017 @default.
- W2890693518 cites W2022049740 @default.
- W2890693518 cites W2024269996 @default.
- W2890693518 cites W2027865074 @default.
- W2890693518 cites W2031037734 @default.
- W2890693518 cites W2035254732 @default.
- W2890693518 cites W2038669354 @default.
- W2890693518 cites W2042506214 @default.
- W2890693518 cites W2042859974 @default.
- W2890693518 cites W2042878866 @default.
- W2890693518 cites W2051249359 @default.
- W2890693518 cites W2053679421 @default.
- W2890693518 cites W2061493364 @default.
- W2890693518 cites W2062066514 @default.
- W2890693518 cites W2062219811 @default.
- W2890693518 cites W2063598701 @default.
- W2890693518 cites W2065008352 @default.
- W2890693518 cites W2066794100 @default.
- W2890693518 cites W2070137502 @default.
- W2890693518 cites W2071223456 @default.
- W2890693518 cites W2073551447 @default.
- W2890693518 cites W2074964089 @default.
- W2890693518 cites W2077530886 @default.
- W2890693518 cites W2077586977 @default.
- W2890693518 cites W2079368483 @default.
- W2890693518 cites W2079820326 @default.
- W2890693518 cites W2080871553 @default.
- W2890693518 cites W2081756657 @default.
- W2890693518 cites W2083925451 @default.
- W2890693518 cites W2086540154 @default.
- W2890693518 cites W2090499387 @default.
- W2890693518 cites W2092519026 @default.
- W2890693518 cites W2093873176 @default.
- W2890693518 cites W2094951393 @default.
- W2890693518 cites W2095795830 @default.
- W2890693518 cites W2096219086 @default.
- W2890693518 cites W2097403132 @default.
- W2890693518 cites W2100330575 @default.
- W2890693518 cites W2107806245 @default.
- W2890693518 cites W2108531121 @default.
- W2890693518 cites W2111820781 @default.
- W2890693518 cites W2120211787 @default.
- W2890693518 cites W2122809335 @default.
- W2890693518 cites W2124757012 @default.
- W2890693518 cites W2125200373 @default.
- W2890693518 cites W2125485522 @default.
- W2890693518 cites W2126333983 @default.
- W2890693518 cites W2136064506 @default.
- W2890693518 cites W2138785184 @default.
- W2890693518 cites W2139897444 @default.
- W2890693518 cites W2145122944 @default.
- W2890693518 cites W2148963585 @default.
- W2890693518 cites W2151593806 @default.
- W2890693518 cites W2151779229 @default.
- W2890693518 cites W2154043231 @default.
- W2890693518 cites W2158569873 @default.
- W2890693518 cites W2158635729 @default.