TY - GEN
T1 - Global wave climate based on the JMA/MRI-AGCM3.2 climate change projection
AU - Zikra, M.
AU - Hashimoto, N.
AU - Ekstedt, J.
AU - Kodama, M.
N1 - Publisher Copyright:
© APAC 2013.All rights reserved.
PY - 2020
Y1 - 2020
N2 - In this study, global wave climates for present and future climates are simulated by the WAM model, based on wind climate data from the JMA/MRI-AGCM3.2 climate change projection. This study is based on two 6-hourly wind data sets, covering two periods of 1979-2003 (present climate) and 2075-2099 (future climate). These wind data are used to run the WAM model for generating output of wave characteristics. The outputs from each period then were used to study global wave climate in the future. It is found that the wave climate is strongly dependent on latitude, with the largest waves, as well as most significant seasonal variations, located at the mid to high latitude regions. These areas are also where the climate induced changes from present to future climate are most noteworthy. The largest increases of significant wave height of approximately +5%, is experienced in the southern parts of the Indian, Pacific and Atlantic Oceans as well as in the Antarctic Ocean. The largest decreases are of the same order, and limited to the northern Atlantic Ocean.
AB - In this study, global wave climates for present and future climates are simulated by the WAM model, based on wind climate data from the JMA/MRI-AGCM3.2 climate change projection. This study is based on two 6-hourly wind data sets, covering two periods of 1979-2003 (present climate) and 2075-2099 (future climate). These wind data are used to run the WAM model for generating output of wave characteristics. The outputs from each period then were used to study global wave climate in the future. It is found that the wave climate is strongly dependent on latitude, with the largest waves, as well as most significant seasonal variations, located at the mid to high latitude regions. These areas are also where the climate induced changes from present to future climate are most noteworthy. The largest increases of significant wave height of approximately +5%, is experienced in the southern parts of the Indian, Pacific and Atlantic Oceans as well as in the Antarctic Ocean. The largest decreases are of the same order, and limited to the northern Atlantic Ocean.
KW - Climate change
KW - WAM model
KW - Wave climate
UR - http://www.scopus.com/inward/record.url?scp=85086080955&partnerID=8YFLogxK
M3 - Conference contribution
AN - SCOPUS:85086080955
T3 - Proceedings of the 7th International Conference on Asian and Pacific Coasts, APAC 2013
SP - 926
EP - 931
BT - Proceedings of the 7th International Conference on Asian and Pacific Coasts, APAC 2013
A2 - Suriamihardja, Dadang A.
A2 - Harianto, Tri
A2 - Abdurrahman, M. Asad
A2 - Rahman, Taufiqur
PB - Hasanuddin University Press
T2 - 7th International Conference on Asian and Pacific Coasts, APAC 2013
Y2 - 24 September 2013 through 26 September 2013
ER -