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Ecosystem Responses of the Subtropical Kaneohe Bay, Hawaii, to Climate Change: A Nitrogen Cycle Modeling Approach

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Abstract

The global coastal zone is characterized by high biological productivity and serves as an important channel through which materials are transferred from land to the open ocean, yet little is known how it will be affected by climate change. Here, we use Kaneohe Bay, Hawaii, a semi-enclosed subtropical embayment partially surrounded by a mountainous watershed and fed by river runoff as an example to explore the potential impact of climate change on the pelagic and benthic cycling of nitrogen. We employ a nine-compartment nitrogen cycle biogeochemical box model and perturb it with a set of four idealized climate scenarios. We find that hydrological changes play a dominant role in determining the ecosystem structure, while temperature changes are more important for the trophic state and stability of the ecosystem. The ecosystem stability against storm events does not significantly change under any scenario. The system remains autotrophic in the future; however, it becomes significantly less autotrophic under drier climate, while it turns slightly more autotrophic under wetter climate. These findings may have implications for other high island watershed and coastal ecosystems in the tropics and subtropics.

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Notes

  1. KECOM written using the software package of STELLA® version 9.1.4. The time step of model runs is 2−13 years (≈ 1.1 h). This time step is chosen to ensure numerical stability in the simulations of the fast N turnover in the modeled food web. The fourth Runge–Kutta method is used for numerical integrations.

  2. When multiple runs using a same emissions scenario are available from a single model, one run is chosen based on visual inspection (Jan Sedlacek, personal communication, 23 November 2012). Selected runs from each model are simply averaged, although weighting among models is an issue of ongoing debate (Knutti 2010).

  3. The current upward trend of the global-mean surface temperature is likely to continue for the next several decades owing to the biogeochemical and physical inertia arising from the long residence time of CO2 in the atmosphere (Archer et al. 2009) as well as the slow heat transfer processes in the ocean (Solomon et al. 2010) even if anthropogenic emissions of greenhouse gases, pollutants, and aerosol precursors are drastically reduced in the near future [(Tanaka and Raddatz 2011); further references therein]. However, while global-mean surface temperatures are projected to increase for the next several decades, how that increase, in turn, influences the regional and local climate pattern germane to Kaneohe Bay is not as well-known.

  4. The precipitation and evaporation parameters are kept at their respective reference levels for the present day (Tanaka and Mackenzie 2005). Changes in these parameters within substantial ranges of ±20 % do not result in any significant adjustments in reservoir sizes (results not shown). Water exchange is far more important in controlling the hydrological budget of the bay.

  5. Except for the first set of experiments, the absolute magnitude and period of the storm perturbation are kept the same as the reference experiment for the present-day condition.

  6. It is generally shown in Table 3 that the directions of changes in reservoir sizes under the future climate scenarios (Fig. 3) can be inferred by linear syntheses of directions of reservoir responses to corresponding individual parameter changes (Figures S2 through S6). However, it is not always so, which is most evident in the results for surface radiation and water temperature (Figures S2 and S3). In particular, the pelagic phytoplankton reservoir exhibits a strong nonlinear response to the cooling (Figure S3e). In the results with respect to water exchange and river runoff, nonlinearity is weaker (Figures S4 and S5) but does appear when these parameters are varied across larger ranges (e.g., up to ±60% changes) (results not shown). The nonlinearities discussed here stem from the nonlinear formula used to describe the radiation and temperature control of biological metabolism (Table 1).

  7. The eigenproperty of the model, which is derived both analytically and numerically (Tanaka 2002; Tanaka and Mackenzie 2005), can then be more utilized in future studies. Eigenproperties of ecosystem models are widely used in the field of mathematical ecology [e.g., (May 1973)] although their limitations in revealing ecosystem stabilities are debated (Neubert and Caswell 1997; Hastings 2004; Verdy and Caswell 2008). To our knowledge, only several empirical modeling studies obtain eigenproperties (Carpenter et al. 1992; Cottingham and Carpenter 1994; Laws 1997; Tanaka and Mackenzie 2005; Montoya et al. 2009).

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Acknowledgments

We thank Eric De Carlo for coordinating the Special Issue honoring the career of Fred Mackenzie. We are grateful for Eric De Carlo, Fred Mackenzie, and two anonymous reviewers for comments and feedbacks during the course of this study. K. Tanaka is thankful for Jan Sedlacek for his technical help for retrieving and plotting the CMIP5 data and for Oliver Stebler for his tips to improve the visual presentation of the model diagram. The photograph used as the background of Fig. 2 is credited for Jennifer O. Reynolds. CRIMP and CRIMP2 projects as well as the NOAA/PMEL Carbon Dioxide Program are acknowledged for the climate data collected at Kaneohe Bay. K. Tanaka is supported by a Marie Curie Intra-European Fellowship within the 7th European Community Framework Programme (Proposal N° 255568 under FP7-PEOPLE-2009-IEF). N. Gruber acknowledges financial support by ETH Zurich. The first author designed and constructed the model KECOM as a part of his master thesis under the guidance of Fred Mackenzie (Tanaka 2002). He is pursuing his research career in the field of Earth system science (Mackenzie 2011) and his Marie Curie Fellowship project aims to elucidate the uncertainty and stability property of a coupled C–N-P biogeochemical cycle model (Ver et al. 1999; Mackenzie et al. 2011; Joos et al. 2013). By taking the opportunity to honor Fred’s career, the first author revisits KECOM and addresses questions related to climate change, which he currently works on [e.g., (Tanaka et al. 2007, 2009, 2012, 2013)].

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Tanaka, K., Guidry, M.W. & Gruber, N. Ecosystem Responses of the Subtropical Kaneohe Bay, Hawaii, to Climate Change: A Nitrogen Cycle Modeling Approach. Aquat Geochem 19, 569–590 (2013). https://doi.org/10.1007/s10498-013-9209-4

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