Reconstruction of 3-D Ocean Chlorophyll a Structure in the Northern Indian Ocean Using Satellite and BGC-Argo Data

被引:9
|
作者
Hu, Qiwei [1 ,2 ]
Chen, Xiaoyan [1 ]
Bai, Yan [1 ]
He, Xianqiang [1 ,3 ]
Li, Teng [1 ]
Pan, Delu [1 ,2 ]
机构
[1] Minist Nat Resources, Inst Oceanog 2, State Key Lab Satellite Ocean Environm Dynam, Hangzhou 310012, Peoples R China
[2] Shanghai Jiao Tong Univ, Sch Oceanog, Shanghai 200240, Peoples R China
[3] Donghai Lab, Zhoushan 316021, Peoples R China
基金
中国国家自然科学基金;
关键词
3-D structure; biogeochemical Argo (BGC-Argo); chlorophyll a (Chla); northern Indian Ocean (NIO); remote sensing; RANDOM FOREST; DRIVEN; BIOMASS; COLOR;
D O I
10.1109/TGRS.2022.3233385
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We present a novel method using satellite and biogeochemical Argo (BGC-Argo) data to retrieve the 3-D structure of chlorophyll alpha (Chla) in the northern Indian Ocean (NIO). The random forest (RF)-based method infers the vertical distribution of Chla using the near-surface and vertical features. The input variables can be divided into three categories: 1) near-surface features acquired by satellite products; 2) vertical physical properties obtained from temperature and salinity profiles collected by BGC-Argo floats; and 3) the temporal and spatial features, i.e., day of the year, longitude, and latitude. The RF-model is trained and evaluated using a large database including 9738 profiles of Chla and temperature-salinity properties measured by BGC-Argo floats from 2011 to 2021, with synchronous satellite-derived products. The retrieved Chla values and the validation dataset (including 1948 Chla profiles) agree fairly well, with R-2= 0.962 , root-mean-square error (RMSE) = 0.012, and mean absolute percent difference (MAPD) = 11.31%. The vertical Chla profile in the NIO retrieved from the RF-model is more accurate and robust compared to the operational Chla profile datasets derived from the neural network and numerical modeling. A major application of the RF-retrieved Chla profiles is to obtain the 3-D Chla structure with high vertical resolution. This will help to quantify phytoplankton productivity and carbon fluxes in the NIO more accurately. We expect that RF-model can be used to develop long-time series products to understand the variability of 3-D Chla in future climate change scenarios.
引用
收藏
页数:13
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