Yang Bo, Fox James, Behrenfeld Michael J, Boss Emmanuel S, Haëntjens Nils, Halsey Kimberly H, Emerson Steven R, Doney Scott C
Department of Environmental Sciences University of Virginia Charlottesville VA USA.
Rosenstiel School of Marine and Atmospheric Science Cooperative Institute for Marine and Atmospheric Studies University of Miami Miami FL USA.
J Geophys Res Biogeosci. 2021 Feb;126(2):e2020JG006116. doi: 10.1029/2020JG006116. Epub 2021 Feb 25.
The C incubation method for net primary production (NPP) has limited spatial/temporal resolution, while satellite approaches cannot provide direct information at depth. With chlorophyll-a and backscatter measurements from BGC-Argo floats, we quantified year-round NPP in the western North Atlantic Ocean using both the Carbon-based Productivity Model (CbPM) and Photoacclimation Productivity Model (PPM). Comparison with NPP profiles from C incubation measurements showed advantages and limitations of both models. CbPM reproduced the magnitude of NPP in most cases. However, in the summer the CbPM-based NPP had a large peak in the subsurface, which was an artifact from the subsurface chlorophyll maximum caused by photoacclimation. PPM avoided the artifacts from photoacclimation, but the magnitude of PPM-derived NPP was smaller than the C result. Different NPP distribution patterns along a North-South transect in the Western North Atlantic Ocean were observed, including higher winter NPP/lower summer NPP in the south, timing differences in NPP seasonal phenology, and different NPP depth distribution patterns in the summer months. Using a 6-months record of concurrent oxygen and bio-optical measurements from two Argo floats, we also demonstrated the ability of Argo floats to obtain estimates of the net community production to NPP ratio, ranging from 0.3 in July to -1.0 in December 2016. Our results highlight the utility of float bio-optical profiles and indicate that environmental conditions (e.g., light availability, nutrient supply) are major factors controlling the seasonality and spatial (horizontal and vertical) distributions of NPP in the western North Atlantic Ocean.
用于净初级生产力(NPP)的C培养方法具有有限的空间/时间分辨率,而卫星方法无法提供深度处的直接信息。利用来自生物地球化学-氩气浮标(BGC-Argo)的叶绿素a和后向散射测量数据,我们使用基于碳的生产力模型(CbPM)和光适应生产力模型(PPM)对北大西洋西部全年的NPP进行了量化。与C培养测量得到的NPP剖面进行比较,显示了两种模型的优缺点。CbPM在大多数情况下能够再现NPP的量级。然而,在夏季,基于CbPM的NPP在次表层出现了一个大峰值,这是由光适应导致的次表层叶绿素最大值产生的假象。PPM避免了光适应产生的假象,但PPM得出的NPP量级小于C测量结果。在北大西洋西部沿南北断面观察到了不同的NPP分布模式,包括南部冬季NPP较高/夏季NPP较低、NPP季节物候的时间差异以及夏季月份不同的NPP深度分布模式。利用来自两个氩气浮标的6个月同步氧气和生物光学测量记录,我们还证明了氩气浮标能够获得净群落生产力与NPP比值的估计值,范围从2016年7月的0.3到12月的-1.0。我们的结果突出了浮标生物光学剖面的实用性,并表明环境条件(如光照可用性、营养供应)是控制北大西洋西部NPP季节性和空间(水平和垂直)分布的主要因素。