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Titlebook: Detecting and Modelling Regional Climate Change; Manola Brunet India,Diego López Bonillo Book 2001 Springer-Verlag Berlin Heidelberg 2001

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樓主: Radiofrequency
41#
發(fā)表于 2025-3-28 16:33:08 | 只看該作者
https://doi.org/10.1007/978-3-531-92334-5 this compilation has been to extend, temporally, the preliminary estimations of the long-term variations and trends of the Catalonian temperature (Brunet, ., 1999). The improved meteorological network for this region, composed of 23 records of non-urban stations, has been used to analyse the 1869–1
42#
發(fā)表于 2025-3-28 22:22:46 | 只看該作者
43#
發(fā)表于 2025-3-28 23:31:21 | 只看該作者
Kenji Rowel Q. Lim,Toshifumi Yokotacorded in observatories located at the medium Ebro river basin. For each season, regional anomaly series have been constructed with the purpose of reflecting the evolution of temperatures in this area. The underlying trends have been extracted by smoothing, and then studied in order to appreciate th
44#
發(fā)表于 2025-3-29 06:40:22 | 只看該作者
45#
發(fā)表于 2025-3-29 09:56:06 | 只看該作者
David S. Greenberg,Yonat Tzur,Hermona Soreqg the second half of the 20. century. To characterise the temporal evolution of these parameters in the Segura River basin (Spain), we obtained the temporal series corresponding to the monthly average of the daily maximum and minimum temperature from an extensive dataset of meteorological stations i
46#
發(fā)表于 2025-3-29 13:51:44 | 只看該作者
47#
發(fā)表于 2025-3-29 19:05:28 | 只看該作者
48#
發(fā)表于 2025-3-29 22:27:03 | 只看該作者
Health Literacy in Digital Worldhat would cover uniformly the study zone and that would have sufficiently long precipitation series to include the 1931–1996 period and be concordant over time. From the corresponding homogeneous series of data, we established precipitation anomaly series, both on the seasonal and annual scale, for
49#
發(fā)表于 2025-3-30 00:34:10 | 只看該作者
50#
發(fā)表于 2025-3-30 04:35:43 | 只看該作者
https://doi.org/10.1007/978-3-031-11565-3statistical approaches are used, one based on the analysis of the entire time series and the other on modelling the extreme event process. The performance of two precipitation indices, SPI and percentiles, has been compared using long, medium and short time scales. We present the results correspondi
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