JpGU-AGU Joint Meeting 2017

講演情報

[EJ] 口頭発表

セッション記号 A (大気水圏科学) » A-CG 大気水圏科学複合領域・一般

[A-CG47] [EJ] 陸域生態系の物質循環

2017年5月25日(木) 09:00 〜 10:30 303 (国際会議場 3F)

コンビーナ:加藤 知道(北海道大学農学研究院)、平野 高司(北海道大学大学院農学研究院)、佐藤 永(海洋研究開発機構 地球表層物質循環研究分野)、平田 竜一(国立環境研究所)、座長:平野 高司(北海道大学大学院農学研究院)

10:00 〜 10:30

[ACG47-05] Effects of extreme events on nitrogen export from forested ecosystems: a review

★招待講演

*大手 信人1尾坂 兼一2勝山 正則3小田 智基4水垣 滋5 (1.京都大学大学院情報学研究科社会情報学専攻、2.滋賀県立大学環境科学部環境生態学科、3.京都大学学際融合教育研究推進センター グローバル生存学大学院連携ユニット、4.東京大学大学院農学生命科学研究科森林科学専攻、5.国立研究開発法人土木研究所寒地土木研究所)

キーワード:極端気候現象、窒素流出、森林生態系

The effects of the extreme event on the nitrogen (N) export from forested catchments are important factors for comprehensive understandings on the mechanisms of ecosystem disturbances and recovery and its prediction under global climate change. Previous related studies on this topic have consisted of many case studies with field observational approach and several prediction studies using simulation models and climate change scenario. Observational studies can be classified roughly into following three categories depending on the degree of the disturbance on ecosystem structures and functions:
1) Cases without geomorphological and biogeochemical disturbances: Structures and functions of catchment ecosystem are not disturbed, although high flow conditions occurs.
2) Cases without geomorphological disturbances, but with biogeochemical disturbances such as the changes in N pool size in soils: Structures and functions of catchment ecosystem are altered but those are recoverable within certain time period.
3) Cases with geomorphological disturbances in addition to biogeochemical disturbances: Structures and functions of catchment ecosystem are irreversibly disturbed by landslide and debris flow.
These variations also depend upon the vulnerability of the catchment structures in aspects of biological and geomorphological properties.
Previously, field researches have scarcely been conducted on the type 3 in the N export context, while many case studies for the types 1 and 2 have been previously performed in temperate regions. The major N form during storm events are determined if the movable pool is dissolved or particulate forms, and spatial distributions of those relative to the pathways of direct runoff. However, the evidencing studies on disturbance of the extreme storm events on the N dynamics (transformations and pool size changes) itself are still limited. Predictive studies have previously been conducted only in the non-monsoon regions of North America. More conditional variations, such as seasonal precipitation patterns, will be needed for future projections of the ecosystem responses in global scale perspective.