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Date of download: 12/24/2017 Copyright © ASME. All rights reserved. From: Comparison Between Frequency Domain and Time Domain Riser Analysis J. Offshore Mech. Arct. Eng. 2012;134(4): doi: / Figure Legend: Sketch of the TDP movement. The middle position B is the static configuration and the other two, A and C, are dynamic instants. The black dots represent the seabed.
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Date of download: 12/24/2017 Copyright © ASME. All rights reserved. From: Comparison Between Frequency Domain and Time Domain Riser Analysis J. Offshore Mech. Arct. Eng. 2012;134(4): doi: / Figure Legend: Sketch of the frequency domain’s boundary condition. The middle position is the static configuration and the other two are dynamic instants.
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Date of download: 12/24/2017 Copyright © ASME. All rights reserved. From: Comparison Between Frequency Domain and Time Domain Riser Analysis J. Offshore Mech. Arct. Eng. 2012;134(4): doi: / Figure Legend: Effective tension envelope comparison for the catenary. Min denotes the minimum values, ave denotes average, and max denotes the maximum values.
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Date of download: 12/24/2017 Copyright © ASME. All rights reserved. From: Comparison Between Frequency Domain and Time Domain Riser Analysis J. Offshore Mech. Arct. Eng. 2012;134(4): doi: / Figure Legend: Results of the catenary in the half wave of the Campos Basin. They show the X, Y, Z, θ, ψ, out-of-plane curvature, in-plane curvature, and effective tension amplitudes in the function of the curvilinear coordinate s. BL denotes the boundary layer results.
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Date of download: 12/24/2017 Copyright © ASME. All rights reserved. From: Comparison Between Frequency Domain and Time Domain Riser Analysis J. Offshore Mech. Arct. Eng. 2012;134(4): doi: / Figure Legend: Results of the lazy-wave in the Campos Basin. They show the X, Y, Z, θ, ψ, out-of-plane curvature, in-plane curvature, and effective tension amplitudes in the function of the curvilinear coordinate s. BL denotes the boundary layer results.
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Date of download: 12/24/2017 Copyright © ASME. All rights reserved. From: Comparison Between Frequency Domain and Time Domain Riser Analysis J. Offshore Mech. Arct. Eng. 2012;134(4): doi: / Figure Legend: Results of the lazy-wave in the Norwegian Sea. They show the X, Y, Z, θ, ψ, out-of-plane curvature, in-plane curvature, and effective tension amplitudes in the function of the curvilinear coordinate s. BL denotes the boundary layer results.
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