首页> 外文期刊>Biogeosciences >Importance of dissolved organic nitrogen in the north Atlantic Ocean in sustaining primary production: a 3-D modelling approach
【24h】

Importance of dissolved organic nitrogen in the north Atlantic Ocean in sustaining primary production: a 3-D modelling approach

机译:在北大西洋维持一次生产中溶解有机氮的重要性:3-D建模方法

获取原文
           

摘要

An eddy-permitting coupled ecosystem-circulation model including dissolvedorganic matter is used to estimate the dissolved organic nitrogen (DON)supply sustaining primary production in the subtropical north Atlantic Ocean.After an analysis of the coupled model performances compared to the data, asensitivity study demonstrates the strong impact of parameter values linkedto the hydrolysis of particulate organic nitrogen and remineralisation ofdissolved organic nitrogen on surface biogeochemical concentrations.The physical transport of dissolved organic nitrogen contributes to maintainthe level of primary production in this subtropical gyre. It is dominated bythe meridional component. We estimate a meridional net input of0.039 molN m−2 yr−1 over the domain (13–35° N and71–40° W) in the subtropical gyre. This supply is driven by theEkman transport in the southern part and by non-Ekman transport (meridionalcurrent components, eddies, meanders and fronts) in the northern part of thesubtropical gyre. At 12° N, our estimate (18 kmolN s−1)confirms the estimation (17.9 kmolN s−1) made by Roussenov etal. (2006) using a simplified biogeochemical model in a large scale model.This DON meridional input is within the range (from 0.05 up to0.24 molN m−2 yr−1) (McGillicuddy and Robinson, 1997; Oschlies,2002) of all other possible mechanisms (mesoscale activity, nitrogenfixation, atmospheric deposition) fuelling primary production in thesubtropical gyre. The present study confirms that the lateral supply ofdissolved organic nitrogen might be important in closing the N budget overthe north Atlantic Ocean and quantifies the importance of meridional input ofdissolved organic nitrogen.
机译:利用包括溶解有机物在内的允许涡流耦合的生态系统循环模型,估算北亚热带副热带地区维持一次生产的溶解有机氮(DON)供应量。 该数据的敏感性研究表明,与颗粒有机氮的水解和溶解的有机氮的再矿化有关的参数值对表面生物地球化学浓度的强烈影响。 溶解的有机氮的物理迁移有助于维持该州的初级生产水平。这个亚热带的回旋。它主要由子午线部分组成。我们估计亚热带回旋区域(13–35°N和71–40°W)的子午线净输入为0.039 molN m -2 yr -1 。这种供应是由亚热带回旋区南部的埃克曼运输和非埃克曼运输(子午流分量,涡流,曲折和前锋)驱动的。在12°N时,我们的估计值(18 kmolN s -1 )证实了Roussenov等人的估计值(17.9 kmolN s -1 )。 (2006年)在大型模型中使用简化的生物地球化学模型。此DON子午线输入范围为(从0.05至0.24 molN m −2 yr -1 (McGillicuddy and Robinson,1997; Oschlies,2002),所有其他可能的机制(中尺度活动,固氮,大气沉积)助长了亚热带回旋区的初级生产。本研究证实,溶解有机氮的侧向供应对于关闭北大西洋北部的氮预算可能很重要,并量化了溶解有机氮子午输入的重要性。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号