Representing ocean biology-induced heating effects in ROMS-based simulations for the Indo-Pacific Ocean

IF 4.6 Q2 MATERIALS SCIENCE, BIOMATERIALS ACS Applied Bio Materials Pub Date : 2024-11-07 DOI:10.3389/fmars.2024.1473208
Wenzhe Zhang, Chuan Gao, Feng Tian, Yang Yu, Hongna Wang, Rong-Hua Zhang
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Abstract

Incident shortwave radiation can penetrate and heat the upper ocean water column, acting to modulate the stratification, vertical mixing and sea surface temperature. As a light-absorbing constituent, ocean chlorophyll (CHL) plays an important role in regulating these processes; however, its heating effect on the ocean state remains controversial and exhibits strong model dependence on ways the solar radiation transmission and the related CHL-induced heating are represented. In this study, we implement a chlorophyll-based two-way coupling between physical and ecological processes within the Regional Ocean Modeling System (ROMS). The bio-physics coupled model performs well in simulating the structure and variability of oceanic physical and ecological fields in the tropical Indo-Pacific region. Three CHL-related heating terms are analyzed based on the model output to diagnose the ocean biology-induced heating effects, namely the shortwave radiation part penetrating out of the base of the mixed layer (ML; Qpen), the portion absorbed within the ML (Qabs), and the rate of temperature change of the ML resulting from the Qabs effects (Rsr). Results show that the spatio-temporal distributions of the three heating terms are mainly determined by the ML depth (MLD). However, Qpen can also be regulated by the euphotic depth (ED), especially in the western-central equatorial Pacific. This moderating effect is particularly evident during El Niño when the ED tends to be greater than the MLD; positive ED anomalies act to enhance the positive Qpen anomalies caused by negative MLD anomalies. For the first time, the bio-heating effects are quantified within the ROMS-based two-way coupling context between the physical submodel and ecological submodel over the tropical Indo-Pacific Ocean, providing a basis for further understanding of the bio-effects and mechanisms. It is expected that the methodology and understanding developed in this study can help explore the chlorophyll-related processes in the ocean and the interactions with the atmosphere.
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在基于 ROMS 的印度洋-太平洋模拟中体现海洋生物诱发的加热效应
入射短波辐射可以穿透并加热海洋上层水柱,从而调节分层、垂直混合和海面温度。作为一种光吸收成分,海洋叶绿素(CHL)在调节这些过程中发挥着重要作用;然而,叶绿素对海洋状态的加热效应仍然存在争议,并且与太阳辐射传输和相关的叶绿素诱导加热的表示方法有很大的模型依赖性。在这项研究中,我们在区域海洋模拟系统(ROMS)中实现了基于叶绿素的物理和生态过程的双向耦合。生物物理耦合模型在模拟热带印度洋-太平洋地区海洋物理和生态场的结构和变化方面表现良好。根据模式输出分析了三个与 CHL 有关的加热项,以诊断海洋生物诱导的加热效应,即从混合层(ML)底部穿出的短波辐射部分(Qpen)、在混合层内吸收的部分(Qabs)以及 Qabs 效应导致的混合层温度变化率(Rsr)。结果表明,这三个加热项的时空分布主要由混合层深度(MLD)决定。不过,Qpen 也受极光深度(ED)的调节,尤其是在赤道太平洋中西部。这种调节作用在厄尔尼诺现象期间尤为明显,因为厄尔尼诺现象期间,ED 往往大于 MLD;ED 的正异常会增强 MLD 负异常引起的 Qpen 正异常。在基于 ROMS 的热带印度洋-太平洋物理子模式和生态子模式双向耦合背景下,首次对生物加热效应进行了量化,为进一步了解生物效应和机制奠定了基础。预计本研究开发的方法和理解有助于探索海洋中与叶绿素有关的过程以及与大气的相互作用。
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来源期刊
ACS Applied Bio Materials
ACS Applied Bio Materials Chemistry-Chemistry (all)
CiteScore
9.40
自引率
2.10%
发文量
464
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