A Climatology of Atmospheric Iron Inputs to the Atlantic Ocean

大西洋大气铁输入的气候学

• 批准号: NE/G000239/1
• 负责人: Alexander Baker
• 金额: $ 6.31万
• 依托单位: University of East Anglia
• 依托单位国家: 英国
• 项目类别: Research Grant
• 财政年份: 2008
• 资助国家: 英国
• 起止时间: 2008 至 无数据
• 项目状态: 已结题
• 来源: https://gtr.ukri.org/projects?ref=NE%2FG000239%2F1
• 关键词: Climatology; Atmospheric; Iron; Inputs; Atlantic

Desert dust can be picked up by strong winds and transported great distances, sometimes thousands of kilometres, through the atmosphere. This process has some interesting effects on the climate of our planet. Iron makes up a small portion of the dust and this element is often in short supply for the plants (phytoplankton) that live in the ocean. Wind-blown dust can be an important source of iron to these organisms in some ocean regions and so dust supply can be linked to phytoplankton growth and the uptake of carbon from the atmosphere that this causes. While in the atmosphere, dust also alters the way that radiation is absorbed or reflect by the planet. It is therefore important to include dust transport in models of the Earth's climate system, but our current understanding of this transport is rather poor. One particular difficulty is the lack of measurements available to help constrain and develop such models. Some long-term monitoring sites provide information on changes in dust transport over time, but they are too few and too widely spaced to give adequate information on spatial variability. The UEA group has recently carried out 10 long-transect crossings of the Atlantic Ocean, sampling the atmosphere for the iron content of aerosol and rain. This is a unique dataset and will allow us to assess the atmospheric input of iron to the Atlantic directly, based on field data, for the first time. The results of our study will be shared directly with modellers at the Hadley Centre and the QUEST Earth System Science programme, so that we can ensure that the benefit of this extra information is passed directly to the modelling community.

沙漠尘埃可以被强风带走，并通过大气层传送到很远的地方，有时甚至数千公里。这个过程对我们星球的气候有一些有趣的影响。铁只占尘埃的一小部分，而这种元素对于生活在海洋中的植物（浮游植物）来说往往是短缺的。在某些海洋区域，风吹尘可能是这些生物体的重要铁来源，因此灰尘供应可能与浮游植物的生长和从大气中吸收碳有关。在大气中时，尘埃还会改变行星吸收或反射辐射的方式。因此，在地球气候系统的模型中包括尘埃输送是很重要的，但我们目前对这种输送的理解相当差。一个特别的困难是缺乏测量，以帮助限制和发展这样的模型。一些长期监测点提供了关于尘埃输送随时间变化的信息，但这些监测点数量太少，间隔太广，无法提供关于空间变异性的充分信息。东英吉利大学的研究小组最近进行了10次穿越大西洋的长断面研究，对大气中的气溶胶和雨水中的铁含量进行了取样。这是一个独特的数据集，将使我们能够根据现场数据首次直接评估大气中铁输入大西洋的情况。我们的研究结果将直接与哈德利中心和QUEST地球系统科学计划的建模人员共享，以便我们能够确保将这些额外信息的好处直接传递给建模社区。

项目成果

Estimation of atmospheric nutrient inputs to the Atlantic Ocean from 50°N to 50°S based on large-scale field sampling: Iron and other dust-associated elements

• DOI: 10.1002/gbc.20062
• 发表时间: 2013-09-01
• 期刊: GLOBAL BIOGEOCHEMICAL CYCLES
• 影响因子: 5.2
• 作者: Baker, A. R.;Adams, C.;Ganzeveld, L.
• 通讯作者: Ganzeveld, L.