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v4-matlab griddata  (MathWorks Inc)


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    MathWorks Inc v4-matlab griddata
    V4 Matlab Griddata, supplied by MathWorks Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
    https://www.bioz.com/product/v4-matlab+griddata/10__1016_slash_j__spasta__2016__07__005-134-1-1
    Average 90 stars, based on 1 article reviews
    v4-matlab griddata - by Bioz Stars, 2026-10
    90/100 stars

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    Article Title: Wavelet nonparametric estimation from strong spatial correlated high-dimensional data
    Article Snippet: Contents lists available at ScienceDirect Spatial Statistics journal homepage: www.elsevier.com/locate/spasta Wavelet nonparametric estimation from strong spatial correlated high-dimensional data M.P.. Frías a, M.D.. Ruiz-Medina b,∗ a Department of Statistics and O.R., University of Jaén, Jaén, Spain b Department of Statistics and O.R., University of Granada, Granada, Spain a r t i c l e i n f o Article history: Received 19 March 2016 Accepted 27 July 2016 Available online xxxx Keywords: Climate change Ocean surface temperature Spatial interpolation Spatial nonparametric penalized regression Spatial wavelet shrinkage estimation Strong spatial correlated high-dimensional data a b s t r a c t This paper addresses the problem of spatial prediction from strong spatial correlated high-dimensional data.



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    bicubic spline interpolation matlab r2009a griddata 'v4' option  (MathWorks Inc)
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    Geographic distribution of (A) the age of early Neolithic archaeological sites and (B) the 503F allele of OCTN1. The contour map in (A) is similar to figure 1A in Balaresque et al. (2010) and is based on the dates of 774 archaeological sites provided in Hassan (1985) and Pinhasi et al. (2005). The contour map in (B) is based on the population frequency of 503F in 85 populations across the Old World (supplementary table S2, Supplementary Material online). The intensity surfaces for the contour maps were generated using <t>bicubic</t> spline <t>interpolation</t> (Matlab <t>r2009a</t> griddata, 'v4' option), followed by truncation of values to fit the ranges indicated in the legends (r2009a). In (B), allele frequencies were averaged for populations located within 1°, and values were not interpolated for regions further than 10° from the nearest frequency data point (gray areas). The allele frequency of 503F in a population and the distance of that population to the nearest early Neolithic site are highly correlated (r2 = 0.44, P = 0.0067, t-test of Spearman’s ρ).
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    Geographic distribution of (A) the age of early Neolithic archaeological sites and (B) the 503F allele of OCTN1. The contour map in (A) is similar to figure 1A in Balaresque et al. (2010) and is based on the dates of 774 archaeological sites provided in Hassan (1985) and Pinhasi et al. (2005). The contour map in (B) is based on the population frequency of 503F in 85 populations across the Old World (supplementary table S2, Supplementary Material online). The intensity surfaces for the contour maps were generated using bicubic spline interpolation (Matlab r2009a griddata, 'v4' option), followed by truncation of values to fit the ranges indicated in the legends (r2009a). In (B), allele frequencies were averaged for populations located within 1°, and values were not interpolated for regions further than 10° from the nearest frequency data point (gray areas). The allele frequency of 503F in a population and the distance of that population to the nearest early Neolithic site are highly correlated (r2 = 0.44, P = 0.0067, t-test of Spearman’s ρ).

    Journal: Molecular Biology and Evolution

    Article Title: Crohn's Disease and Genetic Hitchhiking at IBD5

    doi: 10.1093/molbev/msr151

    Figure Lengend Snippet: Geographic distribution of (A) the age of early Neolithic archaeological sites and (B) the 503F allele of OCTN1. The contour map in (A) is similar to figure 1A in Balaresque et al. (2010) and is based on the dates of 774 archaeological sites provided in Hassan (1985) and Pinhasi et al. (2005). The contour map in (B) is based on the population frequency of 503F in 85 populations across the Old World (supplementary table S2, Supplementary Material online). The intensity surfaces for the contour maps were generated using bicubic spline interpolation (Matlab r2009a griddata, 'v4' option), followed by truncation of values to fit the ranges indicated in the legends (r2009a). In (B), allele frequencies were averaged for populations located within 1°, and values were not interpolated for regions further than 10° from the nearest frequency data point (gray areas). The allele frequency of 503F in a population and the distance of that population to the nearest early Neolithic site are highly correlated (r2 = 0.44, P = 0.0067, t-test of Spearman’s ρ).

    Article Snippet: The intensity surfaces for the contour maps were generated using bicubic spline interpolation (Matlab r2009a griddata, 'v4' option), followed by truncation of values to fit the ranges indicated in the legends (r2009a).

    Techniques: Generated