High resolution atmospheric measurements during high-level horizontal flight leg SP50319h03 with POLAR 5

The data set consists of high resolution airborne measurements that were obtained mainly over Svalbard and near the sea ice edge north of Svalbard on three days in March 2013 during the campaign "SpringTime Atmospheric Boundary Layer Experiment (STABLE). STABLE was led by the Alfred Wegener Institue (AWI) and by the Finnish Meteorological Institute (FMI). The measurements were performed using the POLAR 5 research aircraft, where all research flights of 5-6 hours duration started and ended at Longyearbyen airport. During STABLE, observations focused on the vertical structure of the lower troposphere as well as boundary layer modifications, e.g. during marine cold-air outbreaks and by convection over leads in sea ice. The data set presented here predominantly consists of measurements that were obtained over the Wijdefjorden, which is a North-South oriented fjord with a length of more than 100km in the northern part of Spitsbergen. The measurements were carried out to study the boundary layer structure in the fjord as well as for analyses of the role of the topography on the atmospheric conditions. In its southern part, the fjord was covered by land-fast sea ice until about 72.5km north of the fjord's head. In its northern part, there was open water.

本数据集包含高分辨率航空探测数据，这些数据采集于2013年3月的三天科考飞行中，主要覆盖斯瓦尔巴群岛（Svalbard）及其以北的海冰边缘区域，采集工作依托"春季大气边界层实验（SpringTime Atmospheric Boundary Layer Experiment, STABLE）"项目开展。本次科考由阿尔弗雷德·魏格纳研究所（Alfred Wegener Institute, AWI）与芬兰气象研究所（Finnish Meteorological Institute, FMI）联合主导。探测工作搭载"极地5号（POLAR 5）"科研飞机完成，所有时长5至6小时的科研飞行均以朗伊尔城机场作为起降站点。科考期间，观测重点聚焦于对流层低层的垂直结构以及边界层的变化特征，例如海洋冷爆发事件期间与海冰冰间湖对流过程中的边界层演变。本数据集的核心数据采集于维杰峡湾（Wijdefjorden）——该峡湾呈南北走向，位于斯匹次卑尔根岛北部，全长超过100千米。本次探测旨在研究该峡湾内的大气边界层结构，并分析地形对大气状况的影响效应。该峡湾的南部区域（直至峡湾湾顶以北约72.5千米处）被固定海冰覆盖，北部区域则分布有开阔水域。