ICPR2010 Poster Scale matching of 3D point clouds by finding keyscales with spin images

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Scale matching of 3D point clouds by finding keyscales with spin images Scale matching of 3D point clouds by finding keyscales with spin images T. Tamaki, S. Tanigawa, Y. Ueno, B. Raytchev, K. Kaneda Randomly reduced to 30% points Using normalized Spin images Original size vs 10 times larger one keyscale keyscale keyscale keyscale keyscale keyscale Matching scales! keyscale keyscale Scales are matched Keyscale matching

description

Toru Tamaki, Shunsuke Tanigawa, Yuji Ueno, Bisser Raytchev, Kazufumi Kaneda: "Scale matching of 3D point clouds by finding keyscales with spin images," Proc. of ICPR2010 ; The 20th International Conference on Pattern Recognition, pp. 3480-3483(2010 08), Istanbul Convention & Exhibition Centre, Istanbul, Turkey, 2010/8/23-26.

Transcript of ICPR2010 Poster Scale matching of 3D point clouds by finding keyscales with spin images

Page 1: ICPR2010 Poster Scale matching of 3D point clouds by finding keyscales with spin images

Scale matching of 3D point clouds

by finding keyscales with spin images

Scale matching of 3D point clouds

by finding keyscales with spin images

T. Tamaki, S. Tanigawa, Y. Ueno, B. Raytchev, K. Kaneda

Randomly reduced to 30% points

Using normalized Spin images

Original size vs 10 times larger one

keyscale keyscale

keyscale keyscale

keyscale keyscale

Matching scales!

keyscale

keyscale

Scalesare matched

Keyscalematching

Spin Spin Spliting

Spin Spin Spliting

facility.waseley.networcs.net€¦ · Web viewThe Coriolis effect causes the air to spin upwards around a calm centre eye of the storm. Rising air cools, condenses and storm clouds

facility.waseley.networcs.net€¦ · Web viewThe Coriolis effect causes the air to spin upwards around a calm centre eye of the storm. Rising air cools, condenses and storm clouds

How do clouds form? LECTURE 6, Clouds

How do clouds form? LECTURE 6, Clouds

Carbon-hydrogen Spin-spin Coupling Constants

Carbon-hydrogen Spin-spin Coupling Constants

Artic - porcelanatoliquido.net · 4807126 -free-sky-wallpaper jpg clouds clouds texture6118jpg clouds clouds clouds clouds texture6110.jpg clouds texturE6115jpg clouds texture6120.jpg

Artic - porcelanatoliquido.net · 4807126 -free-sky-wallpaper jpg clouds clouds texture6118jpg clouds clouds clouds clouds texture6110.jpg clouds texturE6115jpg clouds texture6120.jpg

Clouds, Rain, Clouds Again

Clouds, Rain, Clouds Again

Key Poses ICPR2010 - Bilkent Universityduygulu/papers/ICPR2010-KeyPoses.pdf · extract features for action recognition. In some studies motion-based methods [3, 4, 17] are exploited,

Key Poses ICPR2010 - Bilkent Universityduygulu/papers/ICPR2010-KeyPoses.pdf · extract features for action recognition. In some studies motion-based methods [3, 4, 17] are exploited,

Why do clouds turn gray? CLOUDS - mrspruillscience€¦ · Stratus Clouds Stratus clouds are uniform grayish clouds that often cover the entire sky. They resemble fog that does not

Why do clouds turn gray? CLOUDS - mrspruillscience€¦ · Stratus Clouds Stratus clouds are uniform grayish clouds that often cover the entire sky. They resemble fog that does not

Subject: Types of clouds Agata Łazarz. Internet Classification identifies clouds by appearance: heaped clouds (cumulus) layer clouds (stratus) feathery.

Subject: Types of clouds Agata Łazarz. Internet Classification identifies clouds by appearance: heaped clouds (cumulus) layer clouds (stratus) feathery.

types of clouds. Different kinds of clouds lead to ... · Different kinds of clouds lead to different types of weather. Cirrus clouds are the highest group of clouds that form above

types of clouds. Different kinds of clouds lead to ... · Different kinds of clouds lead to different types of weather. Cirrus clouds are the highest group of clouds that form above

The invigoration of deep convective clouds over the ...€¦ · undetectable clouds (the abovementioned small clouds or clouds with weak optical signature) decreases as a function

The invigoration of deep convective clouds over the ...€¦ · undetectable clouds (the abovementioned small clouds or clouds with weak optical signature) decreases as a function

Spin Diffusion NMR For Distance Determination Spin Diffusion Methods in SSNMR 1H-driven X-spin isotropic spin diffusion: Direct 1H spin diffusion: • With 1H evolution and X-spin

Spin Diffusion NMR For Distance Determination Spin Diffusion Methods in SSNMR 1H-driven X-spin isotropic spin diffusion: Direct 1H spin diffusion: • With 1H evolution and X-spin

Clouds Cumulus CU Low clouds - cumuliform -. clouds Cumulus CU Low clouds - cumuliform -

Clouds Cumulus CU Low clouds - cumuliform -. clouds Cumulus CU Low clouds - cumuliform -

Formation of Clouds/Types of Clouds

Formation of Clouds/Types of Clouds

Clouds, Rain, Clouds Againstatic.nsta.org › pdfs › samples › PB330X7web.pdfSummary: “In Clouds, rain, clouds again, the reader receives a simplified picture of the water cycle:

Clouds, Rain, Clouds Againstatic.nsta.org › pdfs › samples › PB330X7web.pdfSummary: “In Clouds, rain, clouds again, the reader receives a simplified picture of the water cycle:

Clouds Finding Out What Clouds Are All About. Cirrus Clouds.

Clouds Finding Out What Clouds Are All About. Cirrus Clouds.

Spin WG Summary - spin experiments -

Spin WG Summary - spin experiments -

Clouds, Clouds, and more Clouds!

Clouds, Clouds, and more Clouds!

Speech Emotion Analysis in Noisy Real-World Environmentcvrr.ucsd.edu/publications/2010/ashish-icpr2010.pdf · Speech Emotion Analysis in Noisy Real-World ... used to calculate the

Speech Emotion Analysis in Noisy Real-World Environmentcvrr.ucsd.edu/publications/2010/ashish-icpr2010.pdf · Speech Emotion Analysis in Noisy Real-World ... used to calculate the

Pulse sequences. Categorization Spin echo Spin echo Conventional spin echoConventional spin echo Fast spin echoFast spin echo Inversion recovery Inversion.

Pulse sequences. Categorization Spin echo Spin echo Conventional spin echoConventional spin echo Fast spin echoFast spin echo Inversion recovery Inversion.