摘要(英) |
In 2020, the South Penghu Marine National Park had experienced sever coral bleaching and may cause coral deaths. It’s an important creature that enrich the biodiversity in the ocean. However, the SST that corals can survive is narrow, and the recovery time is about 10 years. The impact of extreme weather can’t be underestimate, and it is critical to accurately predict SST variations.
In addition to SST, DHW near Penghu achieved the highest level in 2020, the risk of coral bleaching has increased significantly in the past. In this study, the deep learning method, LSTM and CNN, is applied to predict SST, and is already reached 99.22% accuracy.
Penghu was not directly attacked by any typhoon in 2020, so lack of typhoon induced SST cooling effect, may be a reason that large area of coral bleaching. The intensity, wind speed, and the thickness of the ocean mixed layer would cause different degrees of SST cooling. A machine learning model, Random Forest, is established to classify whether this typhoon would cause significant cooling effect. The accuracy of the model is 92.9%, and the EOF analysis provides the most obvious cooling factor.
In addition to analyzing the data, this study also conducted twice site survey in Penghu Marine National Park in 2021, and corals were not affected by obvious coral bleaching. This research establishes SST, DHW prediction model and a typhoon induced SST cooling model, hope to provide forecast information for relevant institutions and contribute to the coral conservation of Penghu Marine National Park. |
參考文獻 |
[1] Barber, R. T. and F. P. Chávez (1986). "Ocean variability in relation to living resources during the 1982–83 El Niño." Nature 319(6051): 279-285.
[2] Breiman, L. (2001). "Random forests." Machine learning 45(1): 5-32.
[3] Breiman, L., et al. (1984). "Cart." Classification and Regression Trees;
Wadsworth and Brooks/Cole: Monterey, CA, USA.
[4] Brown, B. (1997). "Coral bleaching: causes and consequences." Coral reefs
16(1): S129-S138.
[5] Ding, M., et al. (2019). "A gated recurrent unit neural networks based wind
speed error correction model for short-term wind power forecasting."
Neurocomputing 365: 54-61.
[6] Edward, J. P., et al. (2018). "Coral mortality in the Gulf of Mannar, southeastern
India, due to bleaching caused by elevated sea temperature in." Current Science
114(9): 1967.
[7] Glynn, P. W., et al. (2001). "Coral bleaching and mortality in Panama and
Ecuador during the 1997–1998 El Niño–Southern Oscillation event: spatial/temporal patterns and comparisons with the 1982–1983 event." Bulletin of Marine Science 69(1): 79-109.
[8] Goreau, T., et al. (2000). "Conservation of coral reefs after the 1998 global bleaching event." Conservation Biology 14(1): 5-15.
[9] Goreau, T. J. and R. L. Hayes (1994). "Coral bleaching and ocean" hot spots"." Ambio-Journal of Human Environment Research and Management 23(3): 176- 180.
[10] Hochreiter, S. and J. J. N. c. Schmidhuber (1997). "Long short-term memory."9(8): 1735-1780.
[11] Hoegh-Guldberg, O. (1999). "Climate change, coral bleaching and the future of
the world′s coral reefs." Marine and freshwater research 50(8): 839-866.
[12] Hwang, P. A., et al. (2003). "A note on analyzing nonlinear and nonstationary
ocean wave data." Applied Ocean Research 25(4): 187-193.
[13] Jaimes, B. and L. K. Shay (2009). "Mixed Layer Cooling in Mesoscale Oceanic Eddies during Hurricanes Katrina and Rita." Monthly Weather Review 137(12):
4188-4207.
[14] Jokiel, P. L. and S. Coles (1977). "Effects of temperature on the mortality and
growth of Hawaiian reef corals." Marine Biology 43(3): 201-208.
[15] LeCun, Y., et al. (1998). "Gradient-based learning applied to document
recognition." Proceedings of the IEEE 86(11): 2278-2324.
[16] Lin, Y.-C., et al. (2020). "Typhoon Type Index: A New Index for Understanding the Rain or Wind Characteristics of Typhoons and Its Application to Agricultural Losses and Crop Vulnerability." Journal of Applied Meteorology and
Climatology 59(5): 973-989.
[17] Nalley, D., et al. (2016). "Inter-annual to inter-decadal streamflow variability in
Quebec and Ontario in relation to dominant large-scale climate indices." Journal
of hydrology 536: 426-446.
[18] NOAA (2020, 7/22). "Daily Global 5 km Satellite Coral Bleaching Heat Stress
Alert Area." Retrieved 12/21, 2020, from
https://coralreefwatch.noaa.gov/product/5km/index_5km_baa_max_r07d.php.
[19] Peñaflor, E., et al. (2009). "Sea-surface temperature and thermal stress in the
Coral Triangle over the past two decades." Coral reefs 28(4): 841-850.
[20] Pichot, V., et al. (2001). "Wavelet transform of heart rate variability to assess autonomic nervous system activity does not predict arousal from general
anesthesia." Canadian Journal of Anesthesia 48(9): 859-863.
[21] Prasad, T. G. and P. J. Hogan (2007). "Upper-ocean response to Hurricane Ivan in a 1/25° nested Gulf of Mexico HYCOM." Journal of Geophysical Research:
Oceans 112(C4).
[22] Price, J. F. (1981). "Upper ocean response to a hurricane." Journal of Physical
Oceanography 11(2): 153-175.
[23] Qin, Z., et al. (2008). "Characterization of CO2 and water vapor fluxes in a
summer maize field with wavelet analysis." Ecological Informatics 3(6): 397-
409.
[24] Richman, M. B. (1986). "Rotation of principal components." Journal of
climatology 6(3): 293-335.
[25] Sanford, T. B., et al. (1987). "Ocean Response to a Hurricane. Part I:
Observations." Journal of Physical Oceanography 17(11): 2065-2083.
[26] Sharma, A. K., et al. (2018). Analysis on the occurrence of tropical cyclone in the South Pacific region using recurrent neural network with LSTM.
International Conference on Neural Information Processing, Springer.
[27] Timmermann, A., et al. (2018). "El Niño–southern oscillation complexity."
Nature 559(7715): 535-545.
[28] Wada, A., et al. (2014). "Typhoon-induced sea surface cooling during the 2011
and 2012 typhoon seasons: Observational evidence and numerical investigations of the sea surface cooling effect using typhoon simulations." Progress in Earth and Planetary Science 1(1): 1-25.
[29] Wang, J., et al. (2020). "Spatiotemporal characteristics of PM2. 5 concentration in the Yangtze River Delta urban agglomeration, China on the application of big data and wavelet analysis." Science of The Total Environment: 138134.
[30] Wang, X., et al. (2011). "Impact of barrier layer on typhoon-induced sea surface
cooling." Dynamics of Atmospheres and Oceans 52(3): 367-385.
[31] Xie, J., et al. (2019). "An adaptive scale sea surface temperature predicting
method based on deep learning with attention mechanism." 17(5): 740-744.
[32] Yogo, M. (2008). "Measuring business cycles: A wavelet analysis of economic
time series." Economics Letters 100(2): 208-212.
[33] Yu, X., et al. (2020). "A novel method for sea surface temperature prediction
based on deep learning." Mathematical Problems in Engineering 2020.
[34] Zhu, T. and D.-L. Zhang (2006). "The impact of the storm-induced SST cooling
on hurricane intensity." Advances in atmospheric sciences 23(1): 14-22.
[35] 張至維, et al. (2013). 澎湖南方四島海域生態熱點調查與潛點規劃, 海洋國家公園管理處. |