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KOTARO KAWAMATA

  (川又 孝太郎)

Profile Information

Affiliation
Professor, Graduate School of Global Environmental Studies, Sophia University

J-GLOBAL ID
202601006171433744
researchmap Member ID
R000114043

Papers

 7
  • KAWAMATA Kotaro
    Environmental Information Science, 54(3) 58-64, 2025  
  • 川又 孝太郎
    環境技術 = Journal of environmental conservation engineering / 「環境技術」編集委員会 編, 51(1) 17-21, Jan, 2022  
  • Kotaro Kawamata, Masahide Horita
    GROUP DECISION AND NEGOTIATION, 23(3) 401-419, May, 2014  Peer-reviewed
  • KAWAMATA Kotaro, HORITA Masahide
    SOCIOTECHNICA, 9 41-49, 2012  Peer-reviewed
    This paper examines the game theoretic models on international climate change negotiation by comparing the actual negotiation process in Kyoto protocol and post-Kyoto negotiation. It reveals that the model's does not reflect EU's leadership, domestic constrain to countries' negotiation position and ethical issues between developed and developing countries, and importance of people's recognition on benefit from mitigation measures. The paper proposes "matching mechanism" similar to conditional pledges by Australia as effective approaches toward ambitious reduction agreement in climate change.
  • (22) 274-279, Aug, 1994  
    Effect of land use development in a coastal region on heat island phenomenon is studied numerically by an urban climate model that employs the k-e turbulence model and an eddy diffusivity model for the transport of momentum, temperature and moisture in the Eckman layer together with a heat balance model for the surface boundary layer and the soil layer. Numerical simulations are carried out for a simplified terrain which consists of sea and land. Changes in wind velocity, temperature and heat fluxes are discussed for three types of land use, that is land surfaces are 1) covered by grass, 2) urbanized as residential area and 3) further developed in a coastal region as business center. It is clarified in the urbanized area that decrease of latent heat flux and increase of sensible heat flux at urban surface raise temperature in the daytime. Urban canopy intensifies sensible heat transfer, leading to higher air temperature. Sea breeze is blocked by the increased roughness in urbanized zone, resulting in the reduced cooling effect of sea breeze.

Misc.

 9