Risk Assessment and Possible Adaptation of Potato Production in Hokkaido to Climate Change Using a Large Number Ensemble Climate Dataset d4PDF-Reference-Cited by-同舟云学术

Risk Assessment and Possible Adaptation of Potato Production in Hokkaido to Climate Change Using a Large Number Ensemble Climate Dataset d4PDF

Published:2021 Issue:0 Volume:17 Page:24-29
ISSN:1349-6476
Container-title:SOLA
language:en
Short-container-title:SOLA

Author:

Sugawara Kuniyasu¹,Inatsu Masaru²,Shimoda Seiji³,Murakami Keach⁴,Hirota Tomoyoshi⁵

Affiliation:

1. Graduate School of Science, Hokkaido University

2. Faculty of Science and Center for Natural Hazards Research, Hokkaido University

3. Hokkaido Agricultural Research Center, Memuro Research Station, National Agriculture and Food Research Organization

4. Hokkaido Agricultural Research Center, National Agriculture and Food Research Organization

5. Faculty of Agriculture, Kyushu University

Publisher

Meteorological Society of Japan

Subject

Atmospheric Science

Link

https://www.jstage.jst.go.jp/article/sola/17/0/17_2021-004/_pdf

Reference31 articles.

1. Adavi, Z., R. Moradi, A. H. Saeidnejad, M. R. Tadayon, and H. Mansouri, 2018. Assessment of potato response to climate change and adaptation strategies. Scientia Horticulturae, 228, 91-102, doi:10.1016/j.scienta.2017.10.017.

2. Donohue, R. J., M. L. Roderick, T. R. McVicar, and G. D. Farquhar, 2013: Impact of CO₂ fertilization on maximum foliage cover across the globe's warm, arid environments. Geophys. Res. Lett., 40, 3031-3035, doi:10.1002/grl.50563.

3. FAOSTAT, 2020: National yield statistics from the food and agriculture organization database. Roma, Italy. (Available online at: http://www.fao.org/faostat/en/#data/QC, accessed 31 August 2020)

4. Franks, P. J., and co-authors, 2013: Sensitivity of plants to changing atmospheric CO₂ concentration: From the geological past to the next century. New Phytol., 197, 1077-1094, doi:10.1111/nph.12104.

5. Fujita, M., and co-authors, 2019: Precipitation changes in a climate with 2-K surface warming from large ensemble simulations using 60-km global and 20-km regional atmospheric models. Geophys. Res. Lett., 46, 435-442, doi:10.1029/2018GL079885.

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