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Intercomparison of the Extended Reconstructed Sea Surface Temperature v4 and v3b Datasets

机译:扩展重构海表温度v4和v3b数据集的比较

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摘要

Version 4 (v4) of the Extended Reconstructed Sea Surface Temperature (ERSST) dataset is compared with its precedent,the widely used version 3b (v3b).The essential upgrades applied to v4 lead to remarkable differences in the characteristics of the sea surface temperature (SST) anomaly (SSTa) in both the temporal and spatial domains.First,the largest discrepancy of the global mean SSTa values around the 1940s is due to ship-observation corrections made to reconcile observations from buckets and engine intake thermometers.Second,differences in global and regional mean SSTa values between v4 and v3b exhibit a downward trend (around -0.032℃ per decade) before the 1940s,an upward trend (around 0.014℃ per decade) during the period of 1950-2015,interdecadal oscillation with one peak around the 1980s,and two troughs during the 1960s and 2000s,respectively.This does not derive from treatments of the polar or the other data-void regions,since the difference of the SSTa does not share the common features.Third,the spatial pattern of the ENSO-related variability of v4 exhibits a wider but weaker cold tongue in the tropical region of the Pacific Ocean compared with that of v3b,which could be attributed to differences in gap-filling assumptions since the latter features satellite observations whereas the former features in situ ones.This intercomparison confirms that the structural uncertainty arising from underlying assumptions on the treatment of diverse SST observations even in the same SST product family is the main source of significant SST differences in the temporal domain.Why this uncertainty introduces artificial decadal oscillations remains unknown.
机译:扩展重建的海面温度(ERSST)数据集的版本4(V4)与其先例,广泛使用的版本3B(V3B)进行了比较。应用于V4的基本升级导致海面温度的特性差异显着差异( SST)在时间和空间域中的异常(SSTA)。首先,20世纪40年代左右的全球平均SSTA值的最大差异是由于船舶观察校正,以便协调铲斗和发动机进气温计的观察。第二,差异在20世纪40年代之前,V4和V3B之间的全球和区域平均SSTA值在20世纪40年代之前,在1950年至2015年期间,在1950年至2015年期间,趋势(每十年左右约0.032℃),跨越峰值振荡20世纪80年代和20世纪60年代和2000年代的两个小槽。这不是来自极地或其他数据空隙区域的治疗,因为SSTA的差异不共同共同第三,与V3B的热带地区相比,v4的enso相关可变性的空间模式在太平洋的热带地区呈现宽但较弱的寒冷舌头,这可能归因于自后者以来的差距填充假设的差异特征卫星观察,而前者的特征是原位的。这是互相熟悉的,即使在同一SST产品系列中,潜在的SST观察的潜在假设产生的结构不确定性是颞下域中显着差异的主要来源。为什么这种不确定性介绍了人造十二型振荡仍然未知。

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  • 来源
    《中国海洋大学学报(英文版)》 |2018年第2期|209-218|共10页
  • 作者

    WANG Jinping; CHEN Xianyao;

  • 作者单位

    Department of Oceanography, College of Oceanic and Atmospheric Sciences, Ocean University of China,Qingdao 266100, China;

    Physical Oceanography Laboratory/CIMST, Ocean University of China and Qingdao National Laboratory for Marine Science and Technology, Qingdao 266100, China;

  • 收录信息 中国科学引文数据库(CSCD);中国科技论文与引文数据库(CSTPCD);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
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  • 入库时间 2022-08-19 03:49:05
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