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A novel hydrographic gridded data set for the northern Antarctic Peninsula

机译:为北南极半岛的新型水文网集数据集

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The northern Antarctic Peninsula (NAP) is a highly dynamic transitional zone between the subpolarpolar and oceanic-coastal environments, and it is located in an area affected by intense climate change, including intensification and spatial shifts of the westerlies as well as atmospheric and oceanic warming. In the NAP area, the water masses originate mainly from the Bellingshausen and Weddell seas, which create a marked regional dichotomy thermohaline characteristic. Although the NAP area has relatively easy access when compared to other Southern Ocean environments, our understanding of the water masses’ distribution and the dynamical processes affecting the variability of the region is still limited. That limitation is closely linked to the sparse data coverage, as is commonly the case in most Southern Ocean environments. This work provides a novel seasonal three-dimensional high-resolution hydrographic gridded data set for the NAP (version 1), namely the NAPv1.0. Hydrographic measurements from 1990 to 2019 comprising data collected by conductivity, temperature, depth (CTD) casts; sensors from the Marine Mammals Exploring the Oceans Pole to Pole (MEOP) consortium; and Argo floats have been optimally interpolated to produce maps of in situ temperature, practical salinity, and dissolved oxygen at ~ 10 km spatial resolution and 90 depth levels. The water masses and oceanographic features in this regional gridded product are more accurate than other climatologies and state estimate products currently available. The data sets are available in netCDF format at https://doi.org/10.5281/zenodo.4420006 (Dotto et al., 2021). The novel and comprehensive data sets presented here for the NAPv1.0 product are a valuable tool to be used in studies addressing climatological changes in the unique NAP region since they provide accurate initial conditions for ocean models and improve the end of the 20th- and early 21st-century ocean mean-state representation for that area.
机译:北部南极半岛(午睡)是亚帕尔棒球菌和海洋沿海环境之间的高度动态过渡区,它位于受激烈的气候变化影响的地区,包括港口的强化和空间偏移以及大气和海洋变暖。在午睡区,水群主要来自Bellingshausen和Weddell Seas,它创造了一个明显的区域二分热卤化物特征。虽然与其他南洋环境相比,午睡区相对容易进入,但我们对水群分配的理解和影响该地区变异性的动态过程仍然有限。这一限制与稀疏数据覆盖密切相关,因为大多数南部海洋环境中常见的情况。这项工作为NAP(版本1)提供了一种新的季节性三维高分辨率水网集数据集,即NAPv1.0。 1990〜2019年的水文测量包括电导率,温度,深度(CTD)铸造的数据;来自海洋哺乳动物的传感器探索海洋杆到杆(Meop)财团; ARGO浮点已得到最佳插值,以在〜10km的空间分辨率和90个深度水平下产生原位温度,实际盐度和溶解氧的地图。该区域网格产品中的水群和海洋特征比目前可用的其他气候和国家估算产品更准确。数据集以HTTPS://doi.org/10.5281/zenodo.4420006以NetCDF格式提供(Dotto等,2021)。此处为NAPv1.0产品提供的新颖和综合数据集是在研究独特午睡地区的气候变化的研究中使用的有价值的工具,因为它们为海洋模型提供准确的初始条件,并提高20世纪和早期21世纪的海洋意思 - 该地区的陈述。

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