勝てるベッターと負けるベッターの違いは? | ベッティング戦略

������������������������������������������������ 2009�N8��11�� �x�͘p���n�k ������������������������������������������������ 1.�n�k�ɂ‚��� (Earthquake Information) �x�͘p�Ŕ��������n�k�B���C����C�n�k�̔��������O�����n��Ŕ��������B�k���͉����Œ����^�n�k�Ƃ͈قȂ�A����̔��M�ɂ͑����]�T�̂���󋵂ł���B ----------------------------------------------------   2009/08/11,05:07:06.252 34.8022 138.5057 23.4 6.5 w 1.0 ---------------------------------------------------- Table1. Earthquake information. Origin time, Epicentral latitude, longitude, depth, and JMA magnitude from the left.(ref. JMA source mechanism) Fig.1. Event location. 2.�ϑ��_���z (Station Distribution) �k�����͂̊ϑ��_���z�̓o�����X���悭�z�u����Ă���A�k���ʒu����̐��x�͏\���ɂ������B Fig.2. Station Distribution. 3.�ً}�n�k���񔭐M�� (Earthquake Early Warning Report) �n�k������8�b���x�ő��񂪔��M����A�}�O�j�`���[�h�͑����ߏ��]���ł�����̂́A�ő�k�x�\����5��ƂȂ��Ă���A ��ʌ����ً}�n�k���񔭐M�̊�𒴂����B����͔�r�I�����i�K�Ŕ��M���ꂽ�ƍl������B -------------------------------------------------------------------   [01] 09/08/11-05:07:06 5- M5.9 35.0N 138.7E 010km (09/08/11-05:07:14)   [06] 09/08/11-05:07:05 5- M6.3 34.8N 138.5E 020km (09/08/11-05:07:22)   [07] 09/08/11-05:07:05 5+ M6.6 34.8N 138.5E 020km (09/08/11-05:07:30)   [08] 09/08/11-05:07:05 5+ M6.6 34.8N 138.5E 020km (09/08/11-05:07:41)   [09] 09/08/11-05:07:05 5+ M6.6 34.7N 138.5E 010km (09/08/11-05:08:02)   [10] 09/08/11-05:07:05 5+ M6.6 34.7N 138.5E 010km (09/08/11-05:08:08) --------------------------------------------------------------------- �i�����珇�ɏ��ԍ��C�k�����C�ő�\���k�x�C�}�O�j�`���[�h�C �k���ܓx�C�k���o�x�C�k���[���C�d�����\�����j from CEORKA ------------------------------------------------------------------- Table2. Earthquake early warning reports. Information ID, Origin time, Maximum Intensity, JMA magnitude, Epicentral latitude, longitude, depth, and time to issue the report from the left.(ref. The Committee of Earthquake Observation and Research in the Kansai Area) �C�ے��ɂ��ً}�n�k����̓��e 4.��͌��� (Analytical Result) �n�k����P�g�̏���3�b�̎������g�����}�O�j�`���[�h����̌��ʂ��ȉ��Ɏ����B �v�Z���ꂽ�����p�����[�^Tau_c��1�b���܂�ŁA�\�������}�O�j�`���[�h�͎��ۂ̒n�k�����������B -------------------------------------------------------   SZOH430908110507.z 138.495 34.971 1.851 4.818 18.705 6.5   SZO016200908110506 138.311 34.857 1.753 4.458 18.780 6.5   SZO014200908110506 138.374 34.965 1.594 4.928 21.722 6.5   SZOH390908110507.z 138.775 34.795 1.543 5.268 24.700 6.5   SZO005200908110506 138.784 34.755 1.339 5.398 26.017 6.5   SZO013200908110506 138.476 35.041 1.245 5.878 26.631 6.5   SZO018200908110506 138.224 34.740 1.677 6.058 26.680 6.5   SZOH330908110507.z 138.356 35.011 1.056 5.638 26.946 6.5   SZO027200908110506 138.801 34.790 2.034 5.368 27.037 6.5   SZO006200908110506 138.794 34.911 1.583 5.838 29.017 6.5 ------------------------------------------------------- Table3. Analytical results using Tau_c method (Wu and Kanamori, 2005). Station ID, Station longitude, latitude, tauc, P-arrival time, epicentral distance(km) , and magnitude from the left. 5.�ϑ��L�^ (Observed Records) �Z��������z�����n�k�ŁAK-NET�̋L�^�ōő�����x��500Gal���x(Fig.4)�A�ő呬�x��40Kine���x(Fig.5)�ł���B�É��s�암�Ők�x6����ϑ����Ă���(Fig.6)�B �����x�����X�y�N�g���ł́A0.3-0.5�b���x�̃X�y�N�g������z���Ă���A�\�����ւ̉e���͔�r�I�������ƍl������B �ɓ������������Ők�x���傫���n�_�������邪�iFig.7)�A����͖~�n�\���̉e�����󂯂Ă���Ƃ݂���BFig.8�ɂ̓{�[�����O�f�[�^���狁�߂��\�w�n�Ղ̑����x�iARV�j�������Ă��邪�ASZOH42�i�C�P���j�̊ϑ��_�͑����x���傫���A�k�x���z�ƑΉ����Ă���B Fig.3. Acceleration waveforms (EW component). Fig.4. Peak Ground Acceleration. Fig.5. Peak Ground Velocity. Fig.6. JMA Seismic Intensity. Fig.7. JMA Seismic Intensity. Fig.8. ARV (surface soil amplification). Reference Wu, Y. M. and H. Kanamori (2005). Experiment on an onsite early warning method for the Taiwan early warning system, Bull. Seism. Soc. Am., 95, 347-353. �C�ے��̐k�x���A�h�ЉȊw�Z�p��������K-NET,KiK-net�̔g�`�𗘗p���܂����B �ً}�n�k����𔭕\�����n�k�̉�͌��� �R�c�^���@�z�[��