griddata v4 Search Results


griddata v4  (MathWorks Inc)
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MathWorks Inc griddata v4
Griddata V4, 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
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bicubic spline interpolation matlab r2009a griddata 'v4' option  (MathWorks Inc)
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MathWorks Inc bicubic spline interpolation matlab r2009a griddata 'v4' option
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).
Bicubic Spline Interpolation Matlab R2009a Griddata 'v4' Option, 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
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griddata (v4)  (MathWorks Inc)
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MathWorks Inc griddata (v4)
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).
Griddata (V4), 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
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griddata v4 method  (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).
Griddata V4 Method, 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
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biharmonic spline interpolation  (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).
Biharmonic Spline Interpolation, 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
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griddata  (MathWorks Inc)
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MathWorks Inc griddata
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).
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
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interpolation griddata method v4  (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).
Interpolation Griddata Method V4, 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
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matlab’s 2-d interpolation function griddata  (MathWorks Inc)
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MathWorks Inc matlab’s 2-d interpolation function griddata
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).
Matlab’s 2 D Interpolation Function 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
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griddata method  (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).
Griddata Method, 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
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v4-matlab griddata  (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).
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
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biharmonic spline interpolation v4  (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).
Biharmonic Spline Interpolation V4, 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
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v4 matlab griddata  (MathWorks Inc)
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MathWorks Inc v4 matlab griddata
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).
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
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Image Search Results


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