Processing math: 100%
Research article

Observations of the Hawaiian Mesopelagic Boundary Community in Daytime and Nighttime Habitats Using Estimated Backscatter

  • The Hawaiian mesopelagic boundary community is a slope-associated assemblage of micronekton that undergoes diel migrations along the slopes of the islands, residing at greater depths during the day and moving upslope to forage in shallower water at night. The timing of these migrations may be influenced by environmental factors such as moon phase or ambient light. To investigate the movements of this community, we examined echo intensity data from acoustic Doppler current profilers (ADCPs) deployed at shallow and deep sites on the southern slope of Oahu, Hawaii. Diel changes in echo intensity (and therefore in estimated backscatter) were observed and determined to be caused, at least in part, by the horizontal migration of the mesopelagic boundary community. Generalized additive modeling (GAM) was used to assess the impact of environmental factors on the migration timing. Sunset time and lunar illumination were found to be significant factors. Movement speeds of the mesopelagic boundary community were estimated at 1.25–1.99 km h-1 (35–55 cm s-1). The location at which the migrations were observed is the future site of a seawater air conditioning system, which will cause artificial upwelling at our shallow observation site and may cause animal entrainment at the seawater intake near our deep water observation site. This study is the first to observe the diel migration of the mesopelagic boundary community on southern Oahu in both deep and shallow parts of the habitat, and it is also the first to examine migration trends over long time scales, which allows a better assessment of the effects of seasons and lunar illumination on micronekton migrations. Understanding the driving mechanisms of mesopelagic boundary community behavior will increase our ability to assess and manage coastal ecosystems in the face of increasing anthropogenic impacts.

    Citation: Comfort CM, Smith KA, McManus MA, Neuheimer AB, Sevadjian JC, Ostrander CE. Observations of the Hawaiian Mesopelagic Boundary Community in Daytime and Nighttime Habitats Using Estimated Backscatter[J]. AIMS Geosciences, 2017, 3(3): 304-326. doi: 10.3934/geosci.2017.3.304

    Related Papers:

    [1] Yuhua Zhu . A local sensitivity and regularity analysis for the Vlasov-Poisson-Fokker-Planck system with multi-dimensional uncertainty and the spectral convergence of the stochastic Galerkin method. Networks and Heterogeneous Media, 2019, 14(4): 677-707. doi: 10.3934/nhm.2019027
    [2] Karoline Disser, Matthias Liero . On gradient structures for Markov chains and the passage to Wasserstein gradient flows. Networks and Heterogeneous Media, 2015, 10(2): 233-253. doi: 10.3934/nhm.2015.10.233
    [3] L.L. Sun, M.L. Chang . Galerkin spectral method for a multi-term time-fractional diffusion equation and an application to inverse source problem. Networks and Heterogeneous Media, 2023, 18(1): 212-243. doi: 10.3934/nhm.2023008
    [4] Kexin Li, Hu Chen, Shusen Xie . Error estimate of L1-ADI scheme for two-dimensional multi-term time fractional diffusion equation. Networks and Heterogeneous Media, 2023, 18(4): 1454-1470. doi: 10.3934/nhm.2023064
    [5] Yves Achdou, Victor Perez . Iterative strategies for solving linearized discrete mean field games systems. Networks and Heterogeneous Media, 2012, 7(2): 197-217. doi: 10.3934/nhm.2012.7.197
    [6] Hirotada Honda . On Kuramoto-Sakaguchi-type Fokker-Planck equation with delay. Networks and Heterogeneous Media, 2024, 19(1): 1-23. doi: 10.3934/nhm.2024001
    [7] Leqiang Zou, Yanzi Zhang . Efficient numerical schemes for variable-order mobile-immobile advection-dispersion equation. Networks and Heterogeneous Media, 2025, 20(2): 387-405. doi: 10.3934/nhm.2025018
    [8] Yin Yang, Aiguo Xiao . Dissipativity and contractivity of the second-order averaged L1 method for fractional Volterra functional differential equations. Networks and Heterogeneous Media, 2023, 18(2): 753-774. doi: 10.3934/nhm.2023032
    [9] Shui-Nee Chow, Xiaojing Ye, Hongyuan Zha, Haomin Zhou . Influence prediction for continuous-time information propagation on networks. Networks and Heterogeneous Media, 2018, 13(4): 567-583. doi: 10.3934/nhm.2018026
    [10] Ioannis Markou . Hydrodynamic limit for a Fokker-Planck equation with coefficients in Sobolev spaces. Networks and Heterogeneous Media, 2017, 12(4): 683-705. doi: 10.3934/nhm.2017028
  • The Hawaiian mesopelagic boundary community is a slope-associated assemblage of micronekton that undergoes diel migrations along the slopes of the islands, residing at greater depths during the day and moving upslope to forage in shallower water at night. The timing of these migrations may be influenced by environmental factors such as moon phase or ambient light. To investigate the movements of this community, we examined echo intensity data from acoustic Doppler current profilers (ADCPs) deployed at shallow and deep sites on the southern slope of Oahu, Hawaii. Diel changes in echo intensity (and therefore in estimated backscatter) were observed and determined to be caused, at least in part, by the horizontal migration of the mesopelagic boundary community. Generalized additive modeling (GAM) was used to assess the impact of environmental factors on the migration timing. Sunset time and lunar illumination were found to be significant factors. Movement speeds of the mesopelagic boundary community were estimated at 1.25–1.99 km h-1 (35–55 cm s-1). The location at which the migrations were observed is the future site of a seawater air conditioning system, which will cause artificial upwelling at our shallow observation site and may cause animal entrainment at the seawater intake near our deep water observation site. This study is the first to observe the diel migration of the mesopelagic boundary community on southern Oahu in both deep and shallow parts of the habitat, and it is also the first to examine migration trends over long time scales, which allows a better assessment of the effects of seasons and lunar illumination on micronekton migrations. Understanding the driving mechanisms of mesopelagic boundary community behavior will increase our ability to assess and manage coastal ecosystems in the face of increasing anthropogenic impacts.


    In the present paper, we consider numerical solution of the time fractional Fokker-Planck equations (TFFPEs):

    {αtuΔu+p(u)+q(x,t)u=f(x,t),(x,t)Ω×(0,T],u(x,0)=u0(x),xΩ,u(x,t)=0,xΩ,t(0,T], (1.1)

    where ΩRd(d=1,2,3), x=(x1,x2,,xd), u0(x) is smooth on Ω, p:=(p1,p2,,pd) with pi:=pi(x,t)(i=1,2,,d) and q:=q(x,t) are continuous functions. αtu represents the Caputo derivative of order α(0,1). When α=1 in Eq (1.1), the corresponding equations are a class of very useful models of statistical physics to describe some practical phenomena. TFFPEs are widely used in statistical physics to describes the probability density function of position and the evolution of the velocity of a particle, see e.g., [1,2,3,4]. The TFFPEs also represent the continuous limit of a continuous time random walk with a Mittag-Leffler residence time density. For a deeper understanding of TFFPEs, we refer the readers to [5,6]. In addition, the regularity of the solutions of the TFFPE (1.1) can be found in [7].

    For the past few years, many numerical methods were used to solve the TFFPEs. For example, Deng [8] proposed an efficient predictor-corrector scheme. Vong and Wang [9] constructed a compact finite difference scheme. Mahdy [10] used two different techniques to study the approximate solution of TFFPEs, namely the fractional power series method and the new iterative method. Yang et al. [11] proposed a nonlinear finite volume format to solve the two-dimensional TFFPEs. More details can refer to [12,13,14,15]. Besides, it is difficult that analysing the convergence and stability properties of the numerical schemes for TFFPEs, when convective and diffusion terms exist at the same time. In the study of TFFPEs, the conditions imposed on p and q were somewhat restrictive. For example, for solving the one-dimensional TFFPEs, Deng [16] proved the stability and convergence under the conditions that p1 was a monotonically decreasing function and q0. Chen et al. [17] obtained the stability and convergence properties of the method with the conditions that p1 was monotone or a constant and q was a constant.

    To solve the time Caputo fractional equations, one of the keys is the treatment of the Caputo derivative, which raised challenges in both theoretical and numerical aspects. Under the initial singularity of the solutions of the equations, many numerical schemes are only proved to be of τα in temporal direction, e.g., convolution quadrature (CQ) BDF method [18], CQ Euler method [19], uniform L1 method et al. [20,21]. Here τ represents the temporal stepsize. Considering the singularity of solutions, different numerical formats were established to obtain high convergence orders, e.g., the Alikhanov scheme (originally proposed in [22]) and the L1 scheme (see e.g., [23]) by employing the graded mesh (i.e., tn=T(n/K)r,n=1,2,,K, r is mesh parameter). It was proved that the optimal convergence of those methods can be 2 and 2α iff r2/α and r(2α)/α, respectively (see e.g., [24,25,26,27,28,29]). The ¯L1 scheme studied in [30,31,32] was another high-order scheme for Caputo fractional derivative. There were also some fast schemes for Caputo fractional derivative, see [33,34,35,36]. When α was small, the grids at the beginning would become very dense. It may lead to the so-called round-off errors. Recently, taking the small α and the initial singularity into account, Li et al. [37] introduced the transformation s=tα for the time variable, and derived and analyzed the equivalent fractional differential equation. They constructed the TL1 discrete scheme, and obtained that the convergence order of the TL1 scheme is of 2α. Based on the previous research, Qin et al. [38] studied the nonlinear fractional order problem, and established the discrete fractional order Grönwall inequality. Besides, discontinuous Galerkin methods were also effective to solve the similar problems with weak singular solutions [39,40,41].

    Much of the past study of TFFPEs (i.e., in [16,17,42,43]) has been based on many restrictions on q and pi,i=1,2,,d. This reduces the versatility of the equations. In the paper, we consider the more general TFFPE (1.1), i.e., q and pi,i=1,2,,d, are variable coefficients, and q is independent of pi. We draw on the treatment of the Caputo derivative in [37], introduce variable substitution, and construct the TL1 Legendre-Galerkin spectral scheme to solve the equivalent s-fractional equation. For time discreteness, we take into account the initial singularity, and obtain that the optimal convergence order is 2α. In terms of spatial discreteness, unlike other schemes [16,17], which impose restrictions on coefficients, the Legendre-Galerkin spectral scheme does not require pi and q to be constants or to be monotonic. Besides, we obtain the following theoretical results. The order of convergence in L2-norm of the method is exponential order convergent in spatial direction and (2α)-th order convergent in the temporal direction. And the scheme is valid for equations with small parameter α.

    The structure of the paper is as follows. In Section 2, we propose the TL1 Legendre-Galerkin spectral scheme for solving TFFPEs. In Section 3, the detailed proof of our main results is presented. In Section 4, two numerical examples are given to verify our obtained theoretical results. Some conclusion remarks are shown in Section 5.

    We denote Wm,p(Ω) and ||||Wm,p(Ω) as the Sobolev space of any functions defined on Ω and the corresponding Sobolev norm, respectively, where m0 and 1p. Especially, denote L2(Ω):=W0,2(Ω) and Hm(Ω):=Wm,2(Ω). Define C0(Ω) as the space of infinitely differentiable functions which are nonzero only on a compact subset of Ω and H10(Ω) as the completion of C0(Ω). For convenience, denote ||||0:=||||L2(Ω), ||||m:=||||Hm(Ω).

    For simplicity, we suppose that Ω=(1,1)d, and u(x,t)H10(Ω)Hm(Ω) for 0tT. First of all, we introduce TL1 scheme to discrete the Caputo fractional derivative. Introducing the change of variable as follows [21,37,44]:

    t=s1/α,w(x,s)=u(x,s1/α). (2.1)

    By this, then the Caputo derivative of u(x,t) becomes

    αtu(x,t)=1Γ(1α)t0u(x,r)r1(tr)αdr=1Γ(1α)s0w(x,r)r1(s1/αr1/α)αdr=Dαsw(x,s). (2.2)

    Hence, Eq (1.1) can be rewritten as

    Dαsw(x,s)Δw+˜p(w)+˜q(x,s)w=˜f(x,s),(x,s)Ω×(0,Tα], (2.3)
    w(x,s)=0,(x,s)Ω×(0,Tα], (2.4)
    w(x,0)=u0(x),xΩ, (2.5)

    where ˜p=(˜p1,˜p2,,˜pd), ˜pd:=pd(x,s1/α),˜q:=q(x,s1/α), and ˜f(x,s)=f(x,s1/α). Let sn=Tαn/K,n=0,1,,K, and the uniform mesh on [0,Tα] with τs=snsn1. For convenience, Ki, i1 represent the positive constants independent of τs and N, where N represents polynomial degree. In addition, we define the following notations

    ˜pnd:=˜pd(x,sn),˜qn:=˜q(x,sn),˜fn:=˜f(x,sn),
    wn:=w(x,sn),˜pn:=(˜pn1,˜pn2,,˜pnd).

    Applying the TL1 approximation, we have

    Dαswn=1Γ(1α)sn0w(x,r)r1(s1/αnr1/α)αdr=1Γ(1α)nl=1wlwl1τsslsl1dr(s1/αnr1/α)α+Qn=nl=1an,nl(wlwl1)+Qn:=Dατwn+Qn. (2.6)

    Here the coefficients an,nl=1τsΓ(1α)slsl1dr(s1/αnr1/α)α, and Qn represents the truncation error. For more details, we refer to [37,38]. By Eq (2.6), then Eq (2.3) arrives at

    DατwnΔwn+˜pn(wn)+˜qnwn=˜fnQn.

    For spatial discretization, we introduce the following basis functions:

    {ψk(x)}={ψk1(x1)ψk2(x2)ψkd(xd),k1,k2,,kdIN},

    where k=(k1,k2,,kd), IN={0,1,2,,N2}. For ψki(xi),i=1,2,,d, one has

    ψki(xi)=Lki(xi)Lki+2(xi)for kiIN, (2.7)

    where {Lj(x)}Nj=0 are the Legendre orthogonal polynomials, given by the following recurrence relationship [45]:

    {(j+1)Lj+1(x)=(2j+1)xLj(x)jLj1(x)for j1,L0(x)=1,L1(x)=x. (2.8)

    Define the finite-dimensional approximation space

    XN=span{ψk(x),k1,k2,,kdIN},

    where N=(N,N,,Nd). For any function wN(x), write

    wN(x)=k1,k2,,kdINˆwkψk(x).

    By Eqs (2.7) and (2.8), we have

    wN(x)|Ω=0for wN(x)XN.

    Then, the TL1 Legendre-Galerkin spectral scheme is to seek WnXN, such that

    (DατWn,v)+(Wn,v)+(Wn,˜pnv)+(˜qnWn,v)=(˜fn,v)for vXN. (2.9)

    Here W0=πNw0, and πN is the Ritz projection operator given in Lemma 2. For instance, if d=1, we solve Eqs (2.3) and (2.4) by

    A1Dατˆwn+(A2+A3n+A4n)ˆwn=Fn, (2.10)

    where ˆwn=(ˆwn0,ˆwn1,ˆwn2,,ˆwnN2)T, A1j,h=(ψh(x),ψj(x)), j,hIN, A2j,h=(ψh(x),ψj(x)), A3nj,h=(˜pnψh(x),ψj(x)), A4nj,h=(˜qnψh(x),ψj(x)), and Fnj,1=(˜fn,ψj(x)).

    The typical solution of Eq (1.1) meets [18,46,47]

    ||ut(x,t)||0Ctα1,

    then, with the help of the changes of variable (2.1), one has (see e.g., [38])

    ||lwsl(x,s)||0C(1+s1/αl)<,l=1,2, (2.11)

    where C>0 is a constant independent of s and x. From [37, Lemma 2.2] and [38, Lemma 2.1], the solution becomes smoother at the beginning.

    Now, the convergence results of TL1 Legendre-Galerkin spectral scheme (2.9) is given as follows.

    Theorem 1. Assume that ˜q and ~pi,i=1,2,,d, in (2.3) are bounded, and that the unique solution w of Eqs (2.3) and (2.4) satisfying Eq (2.11) and w(x,s)H10(Ω)Hm(Ω). Then, there exist N0>0 and τ0>0 such that when NN0 and τsτ0, Eq (2.9) has a unique solution Wn(n=0,1,,K), which satisfies

    ||wnWn||0K(τ2αs+N1m), (2.12)

    where K>0 is a constant independent of τs and N.

    We will present the detailed proof of Theorem 1 in this section. For this, we first introduce the following several lemmas.

    Lemma 1. [37,38] For n1, we get

    0<an,n1an,n2an,0. (3.1)

    Lemma 2. If we given the Ritz projection operator πN:H10(Ω)XN by

    ((πNww),v)=0forvXN,

    then, one can get that [48]

    ||πNww||lCΩNlm||w||mforwH10(Ω)Hm(Ω)

    with dmN+1, where CΩ>0 is a constant independent of N.

    Lemma 3. [49] For any sK=Tα>0 and given nonnegative sequence {λi}K1i=0, assume that there exists a constant λ>0 independent of τs such that λK1i=0λi. Assume also that the grid function {wn|n0} satisfies

    Dατ(wn)2ni=1λni(wi)2+wn(Qn+ξ)forn1,

    where {Qn|n1} is well defined in Eq (2.6). Then, there exists a constant τs>0 such that, when τsτs,

    wj2Eα(2λsj)[w0+C1(τ2αs+ξ)]for1jK,

    where C1 is a constant and Eα(x)=k=0xkΓ(1+kα).

    We will offer the proof of Theorem 1 in this section. The projection πNwn of the exact solution wn satisfies

    (DατπNwn,v)=(πNwn,v)(πNwn,˜pnv)(˜qnπNwn,v)+(˜fn,v)(Qn,v)(Rn,v)for vXN. (3.2)

    Here Rn=Dατ(wnπNwn)Δ(wnπNwn)+˜pn(wnπNwn)+˜qn(wnπNwn), and Qn is the truncation error for approximating the fractional derivative defined in Eq (2.6).

    The error between numerical solution Wn and exact solution wn can be divided into

    ||wnWn||0||wnπNwn||0+||πNwnWn||0. (3.3)

    Let

    en:=πNwnWnfor n=0,1,,K.

    Subtracting Eq (2.9) from Eq (3.2), we get that

    (Dατen,v)=(en,v)(en,˜pnv)(˜qnen,v)(Qn,v)(Rn,v)for vXN. (3.4)

    Setting v=en in Eq (3.4), we obtain

    (Dατen,en)=(en,en)(en,˜pnen)(˜qnen,en)(Qn,en)(Rn,en). (3.5)

    By Lemma 1, we have

    (Dατen,en)=(nl=1an,nl(elel1),en)=(an,0enn1l=1(an,nl1an,nl)elan,n1e0,en)12(an,0||en||20n1l=1(an,nl1an,nl)||el||20an,n1||e0||20)=12Dατ||en||20. (3.6)

    By Cauchy-Schwartz inequality, one can obtain that

    (en,en)(en,˜pnen)(˜qnen,en)||en||20+K1|(en,en)|+K2||en||20||en||20+||en||20+K214||en||20+K2||en||20(K214+K2)||en||20. (3.7)

    Here K1=max0nK{||˜p(x,sn)||0}, and K2=max0nK{maxxΩ|˜q(x,sn)|}. Similarly, we see that

    (Qn,en)||Qn||0||en||0. (3.8)

    Noting that enXN and by Lemma 2, one has

    ((wnπNwn),en)=0.

    Then

    (Rn,en)=(Dατ(wnπNwn),en)((wnπNwn),en)((wnπNwn),pnen)(˜qn(wnπNwn),en)||Dατ(wnπNwn)||0||en||0+K1||(wnπNwn)||0||en||0+K2||wnπNwn||0||en||0CΩNm||Dατwn||m||en||0+K1CΩN1m||wn||m||en||0+K2CΩNm||wn||m||en||0K3N1m||en||0. (3.9)

    Here K3=max0nK{CΩ||Dατwn||m,K1CΩ||wn||m,K2CΩ||wn||m}, and Lemma 2 is applied. Substituting Eqs (3.6)–(3.9) into Eq (3.5), one gets

    Dατ||en||202(K214+K2)||en||20+2(||Qn||0+K3N1m)||en||0.

    Noting that e0=0 and by Lemma 3, it follows that

    ||en||04K3C1(τ2αs+N1m)Eα(4(K21/4+K2)sn).

    By Eq (3.3), we observe

    ||wnWn||0||wnπNwn||0+||en||0CΩNm||wn||m+4K3C1(τ2αs+N1m)Eα(4(K21/4+K2)sn)K(τ2αs+N1m),

    where K=max0nK{CΩ||wn||m,4K3C1Eα(4(K21/4+K2)sn)}. This completes the proof.

    In this section, two numerical examples are given to verify our theoretical results. We define the maximal L2 error and the convergence order in time, respectively, as

    e(K)=max0nK||wnWn||L2,order=log(e(K1)/e(K2))log(K2/K1). (4.1)

    Example 1. Consider the one-dimensional TFFPEs:

    αtu=uxx2ux+t2u+f(x,t),u(1,1)×(0,1], (4.2)

    where the initial-boundary conditions and the forcing term function f are choosen by the analytical solution

    u(x,t)=(t2+tα)(x3+x5)sin(πx).

    In this case, q is independent of p1, furthermore, p1 and q are not monotone functions.

    We solve this problem with the TL1 Legendre-Galerkin spectral method. Table 1 gives the maximal L2 errors, the convergence orders in time and the CPU times with N=14. The temporal convergence orders are close to 2α in Table 1. For the spatial convergence test, we set K=8192. In Figure 1, we give the errors as a function of N with α=0.3,0.5,0.7 in logarithmic scale. We can observe that the errors indicate an exponential decay.

    Table 1.  Maximal L2 errors, convergence orders in time and CPU times with N=14 for Example 1.
    α=0.1 α=0.3 α=0.5
    K e(K) order CPU(s) e(K) order CPU(s) e(K) order CPU(s)
    4 5.3660e-03 * 1.12e-02 7.5697e-03 * 9.76e-03 8.5571e-03 * 9.92e-03
    16 1.3833e-03 0.98 2.45e-02 1.1574e-03 1.35 2.19e-02 1.3367e-03 1.34 2.25e-02
    64 1.7352e-04 1.50 8.06e-02 1.3606e-04 1.54 7.53e-02 1.8311e-04 1.43 7.40e-02
    256 1.6850e-05 1.68 2.90e-01 1.4476e-05 1.62 3.00e-01 2.3859e-05 1.47 3.01e-01

     | Show Table
    DownLoad: CSV
    Figure 1.  Errors in space with α=0.3,0.5,0.7 and different N for Example 1.

    Example 2. Consider the two-dimensional TFFPEs:

    αtu=Δu+t2x2y2(ux+uy)+(2t2xy2+2t2x2y)u,u(1,1)2×(0,1], (4.3)

    where the initial-boundary conditions and the forcing term function f are choosen by the analytical solution

    u(x,y,t)=Eα(tα)sin(πx)sin(πy).

    Table 2 gives the maximal L2 errors, the convergence orders in time and the CPU times with N=14. The temporal convergence orders are close to 2α in Table 2. For the spatial convergence test, we give the errors as a function of N for α=0.3,0.5,0.7 and K=8192 in Figure 2. We use the logarithmic scale for the error-axis. Again, we observe that the errors indicate an exponential decay.

    Table 2.  Maximal L2 errors, convergence orders in time and CPU times with N=14 for Example 2.
    α=0.3 α=0.5 α=0.7
    K e(K) order CPU(s) e(K) order CPU(s) e(K) order CPU(s)
    32 7.0619e-05 * 2.08e-01 1.7386e-04 * 1.73e-01 3.1316e-04 * 1.69e-01
    256 3.3124e-06 1.47 1.34e+00 9.7836e-06 1.38 1.28e+00 2.3617e-05 1.24 1.31e+00
    2048 1.1965e-07 1.60 1.29e+01 4.6734e-07 1.46 1.28e+01 1.6199e-06 1.29 1.30e+01
    8192 1.2339e-08 1.64 8.59e+01 5.9649e-08 1.48 8.54e+01 2.6824e-07 1.30 8.83e+01

     | Show Table
    DownLoad: CSV
    Figure 2.  Errors in space with α=0.3,0.5,0.7 and different N for Example 2.

    We present a TL1 Legendre-Galerkin spectral method to solve TFFPEs in this paper. The new scheme is convergent with O(τ2αs+N1m), where τs, N and m are the time step size, the polynomial degree and the regularity of the analytical solution, respectively. In addition, this TL1 Legendre-Galerkin spectral method still holds for problems with small α and gives better numerical solutions near the initial time. The new scheme can achieve a better convergence result on a relatively sparse grid point.

    The work of Yongtao Zhou is partially supported by the NSFC (12101037) and the China Postdoctoral Science Foundation (2021M690322).

    The authors declare that they have no conflicts of interest.

    [1] Clarke TA (1973) Some aspects of the ecology of lanternfishes (Myctophidae) in the Pacific Ocean near Hawaii. Fish Bull 71: 403-434.
    [2] Gal G, Loew ER, Rudstam LG, et al. (1999) Light and diel vertical migration: spectral sensitivity and light avoidance by Mysis relicta. Can J Fish Aquat Sci 56: 311-322. doi: 10.1139/f98-174
    [3] Bianchi D, Mislan K (2016) Global patterns of diel vertical migration times and velocities from acoustic data. Limnol Oceanogr 61: 353-364. doi: 10.1002/lno.10219
    [4] Tarling GA, Cuzin-Roudy J, Buchholz F (1999) Vertical migration behaviour in the northern krill Meganyctiphanes norvegica is influenced by moult and reproductive processes. Mar Ecol- Prog Ser 190: 253-262. doi: 10.3354/meps190253
    [5] Salvanes AGV, Kristofersen JB. (2001) Mesopelagic fishes. Encycl Ocean Sci 1711-1717.
    [6] Staby A, Aksnes DL (2011) Follow the light-diurnal and seasonal variations in vertical distribution of the mesopelagic fish Maurolicus muelleri. Mar Ecol – Prog Ser 422: 265-273 . doi: 10.3354/meps08938
    [7] Reid SB, Hirota J, Young RE, et al. (1991) Mesopelagic-boundary community in Hawaii: Micronekton at the interface between neritic and oceanic ecosystems. Mar Biol 109: 427-440. doi: 10.1007/BF01313508
    [8] Porteiro FM, Sutton T (2007) Midwater fish assemblages and seamounts. Seamounts: Ecology, Fisheries, and Conservation 12: 101-116.
    [9] Benoit-Bird KJ, Au WWL (2006) Extreme diel horizontal migrations by a tropical nearshore resident micronekton community. Marine Ecology-Progress Series 319: 1-14. doi: 10.3354/meps319001
    [10] Benoit-Bird KJ, Au WW (2003) Prey dynamics affect foraging by a pelagic predator (Stenella longirostris) over a range of spatial and temporal scales. Behav Ecol Sociobiol 53: 364-373.
    [11] Hays GC (1995) Ontogenetic and seasonal variation in the diel vertical migration of the copepods Metridia lucens and Metridia longa. Limnol oceanog 40: 1461-1465. doi: 10.4319/lo.1995.40.8.1461
    [12] Hays GC (2003) A review of the adaptive significance and ecosystem consequences of zooplankton diel vertical migrations. In: Migrations and dispersal of marine organisms. Springer Netherlands, 503: 163-170.
    [13] Prihartato PK, Aksnes DL, Kaartvedt S (2015) Seasonal patterns in the nocturnal distribution and behavior of the mesopelagic fish Maurolicus muelleri at high latitudes. Mar Ecol-Progs Ser 521: 189-200. doi: 10.3354/meps11139
    [14] Benoit-Bird KJ, Au WW (2004) Diel migration dynamics of an island-associated sound-scattering layer. Deep Sea Res Part I 51: 707-719. doi: 10.1016/j.dsr.2004.01.004
    [15] McManus MA, Benoit-Bird KJ, Woodson CB (2008) Behavior exceeds physical forcing in the diel horizontal migration of the midwater sound-scattering layer in Hawaiian waters. Mar Ecol-Prog Ser 365: 91-101. doi: 10.3354/meps07491
    [16] Benoit-Bird KJ, McManus MA (2012) Bottom-up regulation of a pelagic community through spatial aggregations. Biol lett 8: 813-816. doi: 10.1098/rsbl.2012.0232
    [17] McManus MA, Sevadjian JC, Benoit-Bird KJ, et al. (2012) Observations of thin layers in coastal Hawaiian waters. Estuaries Coasts 35: 1119-1127. doi: 10.1007/s12237-012-9497-8
    [18] Sevadjian J, McManus M, Benoit-Bird K, et al. (2012) Shoreward advection of phytoplankton and vertical re-distribution of zooplankton by episodic near-bottom water pulses on an insular shelf: Oahu, Hawaii. Cont Shelf Res 50: 1-15.
    [19] Benoit-Bird KJ, McManus MA (2014) A critical time window for organismal interactions in a pelagic ecosystem. PLoS ONE 9: e97763. doi: 10.1371/journal.pone.0097763
    [20] Comfort CM, McManus MA, Clark SJ, et al. (2015) Environmental properties of coastal waters in Mamala bay, Oahu, Hawaii, at the future site of a seawater air conditioning outfall. Oceanogr 28: 230-239.
    [21] Deines KL (1999) Backscatter estimation using broadband acoustic Doppler current profilers. Current measurement. Proc IEEE sixth working conf curr measurements 249-253.
    [22] Sevadjian J, McManus M, Pawlak G (2010) Effects of physical structure and processes on thin zooplankton layers in Mamala Bay, Hawaii. Mar Ecol - Prog Ser 409: 95-106. doi: 10.3354/meps08614
    [23] van Haren H (2007) Monthly periodicity in acoustic reflections and vertical motions in the deep ocean. Geophys res lett 34: 12.
    [24] Heywood KJ (1996) Diel vertical migration of zooplankton in the northeast Atlantic. J Plankton Res 18: 163-184. doi: 10.1093/plankt/18.2.163
    [25] Zuur AF, Ieno EN, Elphick CS (2010) A protocol for data exploration to avoid common statistical problems. Methods Ecol Evolut 1: 3-14. doi: 10.1111/j.2041-210X.2009.00001.x
    [26] R Core Team (2015) R: A language and environment for statistical computing. R Foundation for Statistical Computing, Vienna, Austria. https://www.R-project.org.
    [27] Wood SN (2011) Fast stable restricted maximum likelihood and marginal likelihood estimation of semiparametric generalized linear models. J R Stat Soc (B) 73: 3-36. doi: 10.1111/j.1467-9868.2010.00749.x
    [28] Fox J, Weisberg S (2011) An R companion to applied regression, Second edition, Sage, Thousand Oaks, CA.
    [29] Barton K (2015) Mumin: Multi-model inference. R package version 1151.
    [30] Mazerolle MJ (2015) Aiccmodavg: Model selection and multimodel inference based on (q) aic (c). R package version 20-3.
    [31] MATLAB version R2013a. (2013) The MathWorks Inc., Natick, Massachusetts.
    [32] Benoit-Bird KJ, Au WWL, Brainard RE, et al. (2001) Diel horizontal migration of the Hawaiian mesopelagic boundary community observed acoustically. Mar Ecol-Prog Ser 217: 1-14. doi: 10.3354/meps217001
    [33] Clay CS, Medwin H (1977) Acoustical oceanography: principles and applications. Wiley. University of Michigan. 544.
    [34] Eich ML, Merrifield MA, Alford MH (2004) Structure and variability of semidiurnal internal tides in Mamala bay, Hawaii. J Geophys Res: Oceans 109: C5.
    [35] Hamilton P, Singer J, Waddell E (1995) Ocean current measurements. In: Mamala Bay Study Final Report 1. Project MB, 38 pp and appendices.
    [36] Alford MH, Gregg MC, Merrifield MA (2006) Structure, propagation, and mixing of energetic baroclinic tides in Mamala Bay, Oahu, Hawaii. J Phys Oceanography 36: 997-1018. doi: 10.1175/JPO2877.1
    [37] Clark CW, Levy DA (1988) Diel vertical migrations by juvenile sockeye salmon and the antipredation window. Am Nat 131: 271-290. doi: 10.1086/284789
    [38] Bollens SM, Frost BW (1991) Diel vertical migration in zooplankton: Rapid individual response to predators. J Plankton Res 13: 1359-1365. doi: 10.1093/plankt/13.6.1359
    [39] Lampert W (1993) Ultimate causes of diel vertical migration of zooplankton: New evidence for the predator-avoidance hypothesis. In: Diel vertical migration of zooplankton 79-88.
    [40] Ringelberg J (1995) Changes in light intensity and diel vertical migration: A comparison of marine and freshwater environments. J Mar Biol Assoc U K 75: 15-25.
    [41] Ringelberg J (1999) The photobehaviour of Daphnia spp. as a model to explain diel vertical migration in zooplankton. Biol Rev 74: 397-423.
    [42] Klevjer TA, Irigoien X, Røstad A, et al. (2016) Large scale patterns in vertical distribution and behaviour of mesopelagic scattering layers. Sci Rep 6: 19873. doi: 10.1038/srep19873
    [43] Aksnes DL, Røstad A, Kaartvedt S, et al. (2017) Light penetration structures the deep acoustic scattering layers in the global ocean. Sci Adv 3: e1602468.
    [44] Gibson R, Atkinson R, Gordon J (2009) Zooplankton diel vertical migration-a review of proximate control. Oceanography Mar Biol: Annu Rev 47: 77-110.
    [45] Benoit-Bird KJ, Au WW, Wisdoma DW (2009) Nocturnal light and lunar cycle effects on diel migration of micronekton. Limnol Oceanogr 54: 1789-1800.
    [46] Drazen JC, Lisa G, Domokos R (2011) Micronekton abundance and biomass in Hawaiian waters as influenced by seamounts, eddies, and the moon. Deep Sea Res Part I 58: 557-566. doi: 10.1016/j.dsr.2011.03.002
    [47] Kaartvedt S, Knutsen T, Holst JC (1998) Schooling of the vertically migrating mesopelagic fish Maurolicus muelleri in light summer nights. Mar Ecol-Prog Ser 170: 287-290. doi: 10.3354/meps170287
    [48] Frank T, Widder E (2002) Effects of a decrease in downwelling irradiance on the daytime vertical distribution patterns of zooplankton and micronekton. Mar Biol 140: 1181-1193. doi: 10.1007/s00227-002-0788-7
    [49] Pearre S (2003) Eat and run? The hunger/satiation hypothesis in vertical migration: history, evidence and consequences. Biol Rev 78: 1-79.
    [50] Torgersen T, Kaartvedt S (2001) In situ swimming behaviour of individual mesopelagic fish studied by split-beam echo target tracking. ICES J of Mar Sci: J du Conseil 58: 346-354.
    [51] Clarke TA (1980) Diets of fourteen species of vertically migrating mesopelagic fishes in Hawaiian waters. Fish Bull 78: 3.
    [52] Moteki M, Arai M, Tsuchiya K, et al. (2001) Composition of piscine prey in the diet of large pelagic fish in the eastern tropical Pacific ocean. Fish Sci 67: 1063-1074. doi: 10.1046/j.1444-2906.2001.00362.x
    [53] Holland KN, Grubbs RD (2008) Fish visitors to seamounts: Tunas and billfish at seamounts. In: Seamounts: Ecology, Fisheries & Conservation. Blackwell Publishing, Oxford, UK, pp 189-201.
    [54] Honolulu Seawater Air Conditioning LLC (2014) Final environmental impact statement for the proposed Honolulu Seawater Air Conditioning project, Honolulu, Hawai'i. In: Engineers USA Co (ed). Cardno TEC, Inc., Honolulu, HI, 834.
    [55] Comfort CM, Vega L (2011) Environmental assessment for ocean thermal energy conversion in Hawaii: Available data and a protocol for baseline monitoring. OCEANS 2011 IEEE 1-8.
    [56] Vega LA (2002) Ocean thermal energy conversion primer. Mar Technol Soc J 36: 25-35. doi: 10.4031/002533202787908626
    [57] Gartner JV, Sulak KJ, Ross SW, et al. (2008) Persistent near-bottom aggregations of mesopelagic animals along the North Carolina and Virginia continental slopes. Mar Biol 153: 825-841. doi: 10.1007/s00227-007-0855-1
    [58] Cowles DL (2001) Swimming speed and metabolic rate during routine swimming and simulated diel vertical migration of Sergestes similis in the laboratory. Pac Sci 55: 215-226. doi: 10.1353/psc.2001.0021
    [59] Cunningham JJ, Magdol ZE, Kinner NE (2010) Ocean thermal energy conversion: Assessing potential physical, chemical, and biological impacts and risks. Coastal Response Research Center, University of New Hamphsire, Durham, NH, 33 pp and appendices.
  • This article has been cited by:

    1. Yanping Chen, Jixiao Guo, Unconditional error analysis of the linearized transformed L1 virtual element method for nonlinear coupled time-fractional Schrödinger equations, 2025, 457, 03770427, 116283, 10.1016/j.cam.2024.116283
    2. Yongtao Zhou, Mingzhu Li, Error estimate of a transformed L1 scheme for a multi-term time-fractional diffusion equation by using discrete comparison principle, 2024, 217, 03784754, 395, 10.1016/j.matcom.2023.11.010
    3. Asghar Ali, Jamshad Ahmad, Sara Javed, Rashida Hussain, Mohammed Kbiri Alaoui, Muhammad Aqeel, Numerical simulation and investigation of soliton solutions and chaotic behavior to a stochastic nonlinear Schrödinger model with a random potential, 2024, 19, 1932-6203, e0296678, 10.1371/journal.pone.0296678
    4. Zemian Zhang, Yanping Chen, Yunqing Huang, Jian Huang, Yanping Zhou, A continuous Petrov–Galerkin method for time-fractional Fokker–Planck equation, 2025, 03770427, 116689, 10.1016/j.cam.2025.116689
  • Reader Comments
  • © 2017 the Author(s), licensee AIMS Press. This is an open access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0)
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Metrics

Article views(5878) PDF downloads(1006) Cited by(3)

Figures and Tables

Figures(6)  /  Tables(3)

/

DownLoad:  Full-Size Img  PowerPoint
Return
Return

Catalog