Comparison between Atmospheric Reanalysis Models ERA5 and ERA-Interim at the North Antarctic Peninsula Region

被引:17
作者
Hillebrand, Fernando Luis [1 ]
Bremer, Ulisses Franz [2 ]
Arigony-Neto, Jorge [3 ]
da Rosa, Cristiano Niederauer [1 ]
Mendes, Claudio Wilson, Jr. [2 ]
Costi, Juliana [4 ]
de Freitas, Marcos Wellausen Dias [2 ]
Schardong, Frederico [5 ]
机构
[1] Univ Fed Rio Grande do Sul, Remote Sensing Postgrad Program, Porto Alegre, RS, Brazil
[2] Univ Fed Rio Grande do Sul, Inst Geosci, Porto Alegre, RS, Brazil
[3] Fed Univ Rio Grande, Inst Oceanog, Rio Grande, Brazil
[4] Fed Univ Rio Grande, Computat Modeling Postgrad Program, Rio Grande, Brazil
[5] Fed Inst Rio Grande Sul, Dept Educ, Porto Alegre, RS, Brazil
关键词
air temperature; Antarctic; atmospheric pressure; weather stations; KING GEORGE ISLAND; SOUTHERN-HEMISPHERE; WEST ANTARCTICA; ANNULAR MODE; CLIMATE; TRENDS; PERFORMANCE;
D O I
10.1080/24694452.2020.1807308
中图分类号
P9 [自然地理学]; K9 [地理];
学科分类号
0705 ; 070501 ;
摘要
The availability of accurate meteorological data is important for the modeling of atmospheric flows, enabling the understanding of climate change in a given environment over time. Therefore, this study aimed to evaluate the quality of the meteorological data of 2 m temperature (T) and mean sea level pressure (MSLP), obtained through the atmospheric reanalysis models ERA5 and ERA-Interim (ERA-i) in the northern region of the Antarctic Peninsula, covering the period from 1979 to 2018. To carry out the statistical process, local observations from nine weather stations installed in the study region were used, with data available from the Scientific Committee on Antarctic Research. Statistical analysis evaluated Pearson's linear correlation coefficient (R), standard deviation (sigma), normalized bias, normalized mean absolute error, and normalized root mean square error. Regarding the difference in (T) over bar between weather stations and reanalysis models, we found a better result for ERA5 (Delta(T) over bar = -0.34 degrees C) compared to ERA-i (Delta(T) over bar = 0.37 degrees C); however, for the difference in (MSLP) over bar the ERA-i (Delta(MSLP) over bar = -0.04 hPa) presented a better response in relation to ERA5 (Delta(MSLP) over bar = 0.24 hPa). When verifying the local meteorological observations trend, an increase of T in 0.31 degrees C decade(-1) (Esperanza station) and a reduction of MSLP between -0.56 (Bellingshausen station) and -0.80 hPa decade(-1) (Jubany station) were recorded.
引用
收藏
页码:1147 / 1159
页数:13
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