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芬兰北部的雪地覆盖持续时间和关键变量的影响通过基于观察到的雪深度变化的概念框架
Johan Ström1, Jonas Svensson2, Hans Moosmüller3
1Department of Environmental Science, Stockholm University, 106 91 Stockholm, Sweden.
The Science of the total environment
|August 31, 2023
概括
北芬兰的季节性雪覆盖持续时间可以通过新的框架来简化. 影响雪融的主要因素包括降水,温度,太阳辐射和吸光粒子 (LAP).
科学领域:
- 冰层科学 冰层科学
- 大气科学 大气科学
- 环境物理环境物理
背景情况:
- 季节性雪地覆盖的持续时间受到复杂的大气-冰层相互作用的影响.
- 雪地覆盖的时空空间变化是显著的,复杂的预测.
- 了解雪退缩的时间对于气候和水文研究至关重要.
研究的目的:
- 为了简化管理季节性雪地覆盖持续时间的复杂过程.
- 开发一个新的概念框架来参数化雪深变化.
- 量化关键变量对雪地覆盖持续时间的影响.
主要方法:
- 对芬兰北部观测到的雪深变化的大量数据集进行分析.
- 开发一个概念框架,将雪季划分为黑暗和明亮的时期.
- 降低雪深度的参数化使用平均温度,入射短波辐射和吸光粒子 (LAP).
- 将流程简化为两个线性关系,使用新的LAP度增强配方.
主要成果:
- 季节性雪地覆盖的持续时间在每10毫米降水相当的雪量上大约会变化一天.
- 这种降水效应相当于将雪中的LAP度增加一倍.
- 温度和太阳辐射的年间变化可以解释给定降水量下几周的雪地覆盖持续时间的变化.
结论:
- 一个简化的模型有效地捕捉了芬兰北部季节性雪地覆盖持续时间的动态.
- 降水,温度,太阳辐射和LAP是雪融化时间的关键驱动因素.
- 该框架为了解和预测雪地覆盖面对气候变化的反应提供了有价值的工具.
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