skip to main content
US FlagAn official website of the United States government
dot gov icon
Official websites use .gov
A .gov website belongs to an official government organization in the United States.
https lock icon
Secure .gov websites use HTTPS
A lock ( lock ) or https:// means you've safely connected to the .gov website. Share sensitive information only on official, secure websites.


Title: Spectrally simplified approach for leveraging legacy geostationary oceanic observations
The use of multispectral geostationary satellites to study aquatic ecosystems improves the temporal frequency of observations and mitigates cloud obstruction, but no operational capability presently exists for the coastal and inland waters of the United States. The Advanced Baseline Imager (ABI) on the current iteration of the Geostationary Operational Environmental Satellites, termed the R Series (GOES-R), however, provides sub-hourly imagery and the opportunity to overcome this deficit and to leverage a large repository of existing GOES-R aquatic observations. The fulfillment of this opportunity is assessed herein using a spectrally simplified, two-channel aquatic algorithm consistent with ABI wave bands to estimate the diffuse attenuation coefficient for photosynthetically available radiation, K d ( P A R ) . First, anin situABI dataset was synthesized using a globally representative dataset of above- and in-water radiometric data products. Values of K d ( P A R ) were estimated by fitting the ratio of the shortest and longest visible wave bands from thein situABI dataset to coincident,in situ K d ( P A R ) data products. The algorithm was evaluated based on an iterative cross-validation analysis in which 80% of the dataset was randomly partitioned for fitting and the remaining 20% was used for validation. The iteration producing the median coefficient of determination ( R 2 ) value (0.88) resulted in a root mean square difference of 0.319 m −<#comment/> 1 , or 8.5% of the range in the validation dataset. Second, coincident mid-day images of central and southern California from ABI and from the Moderate Resolution Imaging Spectroradiometer (MODIS) were compared using Google Earth Engine (GEE). GEE default ABI reflectance values were adjusted based on a near infrared signal. Matchups between the ABI and MODIS imagery indicated similar spatial variability ( R 2 = 0.60 ) between ABI adjusted blue-to-red reflectance ratio values and MODIS default diffuse attenuation coefficient for spectral downward irradiance at 490 nm, K d ( 490 ) , values. This work demonstrates that if an operational capability to provide ABI aquatic data products was realized, the spectral configuration of ABI would potentially support a sub-hourly, visible aquatic data product that is applicable to water-mass tracing and physical oceanography research.  more » « less
Award ID(s):
1831937
PAR ID:
10468343
Author(s) / Creator(s):
; ;
Publisher / Repository:
Optica Publishing Group
Date Published:
Journal Name:
Applied Optics
Volume:
61
Issue:
27
ISSN:
1559-128X
Page Range / eLocation ID:
7966
Format(s):
Medium: X
Sponsoring Org:
National Science Foundation
More Like this
  1. In this paper we derive the best constant for the following L ∞<#comment/> L^{\infty } -type Gagliardo-Nirenberg interpolation inequality ‖<#comment/> u ‖<#comment/> L ∞<#comment/> ≤<#comment/> C q , ∞<#comment/> , p ‖<#comment/> u ‖<#comment/> L q + 1 1 −<#comment/> θ<#comment/> ‖<#comment/> ∇<#comment/> u ‖<#comment/> L p θ<#comment/> , θ<#comment/> = p d d p + ( p −<#comment/> d ) ( q + 1 ) , \begin{equation*} \|u\|_{L^{\infty }}\leq C_{q,\infty ,p} \|u\|^{1-\theta }_{L^{q+1}}\|\nabla u\|^{\theta }_{L^p},\quad \theta =\frac {pd}{dp+(p-d)(q+1)}, \end{equation*} where parameters q q and p p satisfy the conditions p > d ≥<#comment/> 1 p>d\geq 1 , q ≥<#comment/> 0 q\geq 0 . The best constant C q , ∞<#comment/> , p C_{q,\infty ,p} is given by C q , ∞<#comment/> , p = θ<#comment/> −<#comment/> θ<#comment/> p ( 1 −<#comment/> θ<#comment/> ) θ<#comment/> p M c −<#comment/> θ<#comment/> d , M c ∫<#comment/> R d u c , ∞<#comment/> q + 1 d x , \begin{equation*} C_{q,\infty ,p}=\theta ^{-\frac {\theta }{p}}(1-\theta )^{\frac {\theta }{p}}M_c^{-\frac {\theta }{d}},\quad M_c≔\int _{\mathbb {R}^d}u_{c,\infty }^{q+1} dx, \end{equation*} where u c , ∞<#comment/> u_{c,\infty } is the unique radial non-increasing solution to a generalized Lane-Emden equation. The case of equality holds when u = A u c , ∞<#comment/> ( λ<#comment/> ( x −<#comment/> x 0 ) ) u=Au_{c,\infty }(\lambda (x-x_0)) for any real numbers A A , λ<#comment/> > 0 \lambda >0 and x 0 ∈<#comment/> R d x_{0}\in \mathbb {R}^d . In fact, the generalized Lane-Emden equation in R d \mathbb {R}^d contains a delta function as a source and it is a Thomas-Fermi type equation. For q = 0 q=0 or d = 1 d=1 , u c , ∞<#comment/> u_{c,\infty } have closed form solutions expressed in terms of the incomplete Beta functions. Moreover, we show that u c , m →<#comment/> u c , ∞<#comment/> u_{c,m}\to u_{c,\infty } and C q , m , p →<#comment/> C q , ∞<#comment/> , p C_{q,m,p}\to C_{q,\infty ,p} as m →<#comment/> + ∞<#comment/> m\to +\infty for d = 1 d=1 , where u c , m u_{c,m} and C q , m , p C_{q,m,p} are the function achieving equality and the best constant of L m L^m -type Gagliardo-Nirenberg interpolation inequality, respectively. 
    more » « less
  2. We prove a single-value version of Reshetnyak’s theorem. Namely, if a non-constant map f W l o c 1 , n ( Ω , R n ) f \in W^{1,n}_{\mathrm {loc}}(\Omega , \mathbb {R}^n) from a domain Ω R n \Omega \subset \mathbb {R}^n satisfies the estimate | D f ( x ) | n K J f ( x ) + Σ ( x ) | f ( x ) y 0 | n \lvert Df(x) \rvert ^n \leq K J_f(x) + \Sigma (x) \lvert f(x) - y_0 \rvert ^n at almost every x Ω x \in \Omega for some K 1 K \geq 1 , y 0 R n y_0\in \mathbb {R}^n and Σ L l o c 1 + ε ( Ω ) \Sigma \in L^{1+\varepsilon }_{\mathrm {loc}}(\Omega ) , then f 1 { y 0 } f^{-1}\{y_0\} is discrete, the local index i ( x , f ) i(x, f) is positive in f 1 { y 0 } f^{-1}\{y_0\} , and every neighborhood of a point of f 1 { y 0 } f^{-1}\{y_0\} is mapped to a neighborhood of y 0 y_0 . Assuming this estimate for a fixed K K at every y 0 R n y_0 \in \mathbb {R}^n is equivalent to assuming that the map f f is K K -quasiregular, even if the choice of Σ \Sigma is different for each y 0 y_0 . Since the estimate also yields a single-value Liouville theorem, it hence appears to be a good pointwise definition of K K -quasiregularity. As a corollary of our single-value Reshetnyak’s theorem, we obtain a higher-dimensional version of the argument principle that played a key part in the solution to the Calderón problem. 
    more » « less
  3. We formulate and prove a Conner–Floyd isomorphism for the algebraic K-theory of arbitrary qcqs derived schemes. To that end, we study a stable ∞<#comment/> \infty -category of non- A 1 \mathbb {A}^1 -invariant motivic spectra, which turns out to be equivalent to the ∞<#comment/> \infty -category of fundamental motivic spectra satisfying elementary blowup excision, previously introduced by the first and third authors. We prove that this ∞<#comment/> \infty -category satisfies P 1 \mathbb {P}^1 -homotopy invariance and weighted A 1 \mathbb {A}^1 -homotopy invariance, which we use in place of A 1 \mathbb {A}^1 -homotopy invariance to obtain analogues of several key results from A 1 \mathbb {A}^1 -homotopy theory. These allow us in particular to define a universal oriented motivic E ∞<#comment/> \mathbb {E}_\infty -ring spectrum M G L \mathrm {MGL} . We then prove that the algebraic K-theory of a qcqs derived scheme X X can be recovered from its M G L \mathrm {MGL} -cohomology via a Conner–Floyd isomorphism\[ M G L ∗<#comment/> ∗<#comment/> ( X ) ⊗<#comment/> L Z [ β<#comment/> ±<#comment/> 1 ] ≃<#comment/> K ∗<#comment/> ∗<#comment/> ( X ) , \mathrm {MGL}^{**}(X)\otimes _{\mathrm {L}{}}\mathbb {Z}[\beta ^{\pm 1}]\simeq \mathrm {K}{}^{**}(X), \]where L \mathrm {L}{} is the Lazard ring and K p , q ( X ) = K 2 q −<#comment/> p ( X ) \mathrm {K}{}^{p,q}(X)=\mathrm {K}{}_{2q-p}(X) . Finally, we prove a Snaith theorem for the periodized version of M G L \mathrm {MGL}
    more » « less
  4. We consider minimizing harmonic maps u u from Ω<#comment/> ⊂<#comment/> R n \Omega \subset \mathbb {R}^n into a closed Riemannian manifold N \mathcal {N} and prove: 1. an extension to n ≥<#comment/> 4 n \geq 4 of Almgren and Lieb’s linear law. That is, if the fundamental group of the target manifold N \mathcal {N} is finite, we have\[ H n −<#comment/> 3 ( sing ⁡<#comment/> u ) ≤<#comment/> C ∫<#comment/> ∂<#comment/> Ω<#comment/> | ∇<#comment/> T u | n −<#comment/> 1 d H n −<#comment/> 1 ; \mathcal {H}^{n-3}(\operatorname {sing} u) \le C \int _{\partial \Omega } |\nabla _T u|^{n-1} \,\mathrm {d}\mathcal {H}^{n-1}; \]2. an extension of Hardt and Lin’s stability theorem. Namely, assuming that the target manifold is N = S 2 \mathcal {N}=\mathbb {S}^2 we obtain that the singular set of u u is stable under small W 1 , n −<#comment/> 1 W^{1,n-1} -perturbations of the boundary data. In dimension n = 3 n=3 both results are shown to hold with weaker hypotheses, i.e., only assuming that the trace of our map lies in the fractional space W s , p W^{s,p} with s ∈<#comment/> ( 1 2 , 1 ] s \in (\frac {1}{2},1] and p ∈<#comment/> [ 2 , ∞<#comment/> ) p \in [2,\infty ) satisfying s p ≥<#comment/> 2 sp \geq 2 . We also discuss sharpness. 
    more » « less
  5. Consider the Vlasov–Poisson–Landau system with Coulomb potential in the weakly collisional regime on a 3 3 -torus, i.e. ∂<#comment/> t F ( t , x , v ) + v i ∂<#comment/> x i F ( t , x , v ) + E i ( t , x ) ∂<#comment/> v i F ( t , x , v ) = ν<#comment/> Q ( F , F ) ( t , x , v ) , E ( t , x ) = ∇<#comment/> Δ<#comment/> −<#comment/> 1 ( ∫<#comment/> R 3 F ( t , x , v ) d v −<#comment/> ∫<#comment/> −<#comment/> T 3 ∫<#comment/> R 3 F ( t , x , v ) d v d x ) , \begin{align*} \partial _t F(t,x,v) + v_i \partial _{x_i} F(t,x,v) + E_i(t,x) \partial _{v_i} F(t,x,v) = \nu Q(F,F)(t,x,v),\\ E(t,x) = \nabla \Delta ^{-1} (\int _{\mathbb R^3} F(t,x,v)\, \mathrm {d} v - {{\int }\llap {-}}_{\mathbb T^3} \int _{\mathbb R^3} F(t,x,v)\, \mathrm {d} v \, \mathrm {d} x), \end{align*} with ν<#comment/> ≪<#comment/> 1 \nu \ll 1 . We prove that for ϵ<#comment/> > 0 \epsilon >0 sufficiently small (but independent of ν<#comment/> \nu ), initial data which are O ( ϵ<#comment/> ν<#comment/> 1 / 3 ) O(\epsilon \nu ^{1/3}) -Sobolev space perturbations from the global Maxwellians lead to global-in-time solutions which converge to the global Maxwellians as t →<#comment/> ∞<#comment/> t\to \infty . The solutions exhibit uniform-in- ν<#comment/> \nu Landau damping and enhanced dissipation. Our main result is analogous to an earlier result of Bedrossian for the Vlasov–Poisson–Fokker–Planck equation with the same threshold. However, unlike in the Fokker–Planck case, the linear operator cannot be inverted explicitly due to the complexity of the Landau collision operator. For this reason, we develop an energy-based framework, which combines Guo’s weighted energy method with the hypocoercive energy method and the commuting vector field method. The proof also relies on pointwise resolvent estimates for the linearized density equation. 
    more » « less