Interhemispheric high-frequency geomagnetic field dynamics

半球间高频地磁场动力学

• 批准号: RGPIN-2017-05294
• 负责人: StOnge, Guillaume
• 金额: $ 3.42万
• 依托单位: Université du Québec à Rimouski
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2022
• 资助国家: 加拿大
• 起止时间: 2022-01-01 至 2023-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=765292
• 关键词: Interhemispheric; frequency; geomagnetic; field; dynamics

Recent direct observations have demonstrated that the geomagnetic field has undergone dramatic changes over the last century. This is best illustrated by changes in the position of the North Magnetic Pole (NMP) and the rapid decline of the dipole field (i.e, the main component of Earth's magnetic field). The NMP, restricted to the Canadian Arctic during historical times (last 400 yrs), has recently moved into the Arctic Ocean. Direct observations reveal that the migration of the NMP has increased dramatically since the early 1970's from 9 km/yr to 41 km/yr and to almost 60 km/yr in 2003, whereas the annual rate of change in intensity measured at the Resolute Bay geomagnetic observatory has increased from about 10 nT/yr to almost 70 nT/yr over the last 50 years. In addition, the recent migration of the NMP occurs between two important areas of observed geomagnetic fluxes in North America and Siberia. The role of these geomagnetic flux lobes in driving Holocene geomagnetic variability is currently unknown, but maybe key. Similarly, recent satellite observations in the Southern Hemisphere and geomagnetic models reveal an important magnetic anomaly developed over the last centuries in the Southern Hemisphere. The origin and cause of this anomaly, named the South Atlantic Magnetic Anomaly are still unknown. These recent spectacular changes lead to the formulation of the following questions: “Are we in the initial stages of a large-scale geomagnetic change, or even a reversal?” and “are these changes associated with the dynamics of flux lobes?”. To answer these fundamental questions, the historical record must first be placed into a longer geological context. The long-term goal of my Discovery Grant program is to determine the high frequency dynamics of the geomagnetic field during the Late Quaternary with a special emphasis on abrupt changes in the high latitudes of both hemispheres. This research program will provide the first large-scale Holocene interhemispheric study of high latitude geomagnetic field dynamics. In addition, by selecting coring sites with very high sediment accumulation rates, the proposed research will investigate geomagnetic field variability at a temporal resolution that is just beginning to be explored, the centennial to millennial timescales. These observations will: 1) enable testing of hypotheses developed from the historical geomagnetic record, 2) yield invaluable data for geodynamo modelling, and 3) place the current dramatic collapse and migration of the NMP into a detailed geological context. The proposed research will also provide novel data to enhance our understanding of Sun/Earth interactions, as the combination of paleomagnetic and 10Be analysis from the same cores will help decipher the influence of the geomagnetic field on the production rate of cosmogenic isotopes, with practical implications for dating, space weather, telecommunications and climate.

最近的直接观测表明，地磁场在上个世纪经历了巨大的变化。北磁极（NMP）位置的变化和偶极场（即地球磁场的主要组成部分）的快速下降最能说明这一点。在历史时期（过去400年），NMP仅限于加拿大北极地区，最近已进入北冰洋。直接观测表明，自20世纪70年代初以来，NMP的迁移急剧增加，从9公里/年增加到41公里/年，2003年增加到近60公里/年，而在Resolute Bay地磁观测站测量的强度年变化率在过去50年中从约10 nT/年增加到近70 nT/年。此外，NMP最近的迁移发生在北美和西伯利亚两个重要的地磁观测区之间。这些地磁通量波瓣在驱动全新世地磁变化中的作用目前尚不清楚，但可能是关键。同样，最近对南半球的卫星观测和地磁模型显示，南半球在过去几个世纪中出现了一种重要的磁异常。这种被称为南大西洋磁异常的异常的起源和原因仍然未知。这些最近的壮观变化导致了以下问题的形成：“我们是否处于大规模地磁变化的初始阶段，甚至是逆转？”以及“这些变化是否与通量瓣的动力学有关？"。要回答这些基本问题，必须首先将历史记录置于更长的地质背景中。我的发现资助计划的长期目标是确定晚第四纪地磁场的高频动态，特别强调两个半球高纬度地区的突然变化。这项研究计划将提供第一个大规模的全新世半球间研究高纬度地磁场动力学。此外，通过选择沉积物积累率非常高的取芯地点，拟议的研究将以刚刚开始探索的时间分辨率，即百年至千年的时间尺度，调查地磁场的变化。这些意见将：1）能够测试从历史地磁记录中得出的假设，2）为地球发电机建模提供宝贵的数据，3）将NMP当前的急剧崩溃和迁移置于详细的地质背景中。拟议的研究还将提供新的数据，以提高我们对太阳/地球相互作用的理解，因为来自相同核心的古地磁和10 Be分析的结合将有助于破译地磁场对宇宙成因同位素生产率的影响，对测年，空间天气，电信和气候具有实际意义。