Marine Ecosystems Research Department - jamstec japan agency ...
Marine Ecosystems Research Department - jamstec japan agency ...
Marine Ecosystems Research Department - jamstec japan agency ...
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Japan <strong>Marine</strong> Science and Technology Center<br />
Frontier <strong>Research</strong> System for Global Change<br />
than many earlier ones. Nitrous oxide, and ammonia<br />
emission from animal farming of South, Southeast, and<br />
East Asia, in , was estimated at about . Tg<br />
N O_N and . Tg NH _N, respectively, For providing<br />
spatial distributions of these gases, the emissions of<br />
county and district level were allocated into each<br />
.˚grid by means of weighting by high-resolution land<br />
cover data sets.<br />
Fig. 13 Difference in CO monthly mean total column amounts<br />
between Moshiri /Rikubetsu stations (Hokkaido, Japan)<br />
and Zvenigorod station (near Moscow, Russia) (blue) compared<br />
with calculated contributions from forest fire emissions<br />
(red) and incomplete combustion of wood and oil<br />
products (black).<br />
urements at a tropical rural site in Thailand show<br />
strong seasonal cycles with a peak in the late-dry season<br />
(February-March) and a valley in mid-wet season<br />
(June-August). Analysis of air mass trajectories and<br />
ATSR satellite hot spots data verify that the high O <br />
and CO observed in continental SE Asia are caused<br />
mainly by the regional-scale biomass burning. Longrange<br />
transport of regionally polluted continental air<br />
from East Asia also partly contributes to these high O <br />
and CO levels. Meanwhile, the low O and CO in the<br />
wet season are due to the inflow of clean marine air<br />
masses from the Indian Ocean.<br />
Long-term ozonesonde data (-) for tropospheric<br />
ozone from central Europe and East Asia have<br />
been analyzed using the isentropic backward trajectories.<br />
It was shown that photochemically aged boundary layer<br />
ozone reflects the NOx emission trend in each continent.<br />
We collected data of most of the field studies on<br />
methane emission from rice fields available so far in<br />
mainland China. Based on these region-specific emission<br />
factors and statistical data on rice areas of ,<br />
we estimated CH emission from rice fields during the<br />
rice-growing season (from transplanting to harvest) in<br />
Mainland China to be . Tg yr - , with a range of .<br />
to . Tg CH yr - . This estimate is significantly lower<br />
5. Ecosystem Change <strong>Research</strong> Program<br />
One of the most important research subjects of today<br />
is investigating the influence of climate and environmental<br />
changes such as global warming and desertification<br />
on species distribution and diversities. For this<br />
mission, the objective of the Ecosystem Change<br />
<strong>Research</strong> Program (ECRP) is to research on evaluation<br />
of the influences of climate and environmental changes<br />
on ecosystems and modeling their mechanisms.<br />
Conversely, the influence of ecosystem changes on climate<br />
and the environment are evaluated and their<br />
mechanisms are modeled. Our program consists of the<br />
following four groups, studying environmental dynamics<br />
and conducting research on modeling dynamics.<br />
a. Ecosystem-Atmospheric Interaction Model Group<br />
b. Ecosystem Architecture Model Group<br />
c. Ecosystem Geographical Distribution Model Group<br />
d. <strong>Marine</strong> Biological Process Model Group<br />
In FY , we started the detection of ecosystem<br />
change on land and in the ocean by satellite remote<br />
sensing. ECRP also launched research on the integration<br />
of remote sensing with modeling to improve the<br />
model simulation accuracy.<br />
a. Ecosystem-Atmosphere Interaction Model Group<br />
We have been developing a simulation model of carbon<br />
cycle in land ecosystems (Sim-CYCLE). In<br />
FY, we extended to account for the atmospherebiosphere<br />
exchange of stable carbon isotope composition<br />
(δ C). Global simulation showed average fraction-<br />
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