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PIK Biennial Report 2000-2001 - Potsdam Institute for Climate ...

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Goal<br />

To study the role of the land biosphere as a provider of<br />

the human environment and services and as part of the<br />

coupled physical and biogeochemical Earth system, on<br />

the time-scale of historic and future human intervention,<br />

i.e. years to a few centuries.<br />

Research Questions<br />

In this project, we address the following questions:<br />

(a) What is the current and future structure and function<br />

of the land biosphere as a provider of the human environment<br />

and services?<br />

(b) What is the current and future role of the land biosphere<br />

as part of the coupled Earth system on the<br />

(“human”) time-scale of years to a few centuries?<br />

Fig. 3: Interannual Terrestrial carbon exchange anomalies (from<br />

the 1980-98 mean) using the bottom-up LPJ-DGVM approach<br />

(red), compared against top-down atmospheric inversion. Mean<br />

inversion is in black (Bousquet, Peylin, LSCE), the range of 20<br />

inversions (grey).<br />

Tools and development<br />

The Lund-<strong>Potsdam</strong>-Jena Dynamic Global Vegetation<br />

Model (LPJ-DGVM) is one of the world’s leading models<br />

of the global biospheric carbon cycle and of vegetation<br />

dynamics. Continued development of key components<br />

of the model, their validation with observed<br />

ecosystem data on several scales, and the study of the<br />

EVITA<br />

Exergy, Vegetation and In<strong>for</strong>mation: Thermodynamics Approach<br />

Project speaker: Yuri Svireshev<br />

<strong>PIK</strong> project members: W. Steinborn<br />

External project collaborators: Kiel Ecology Centre<br />

past and future of the global carbon cycle are the current<br />

focus of <strong>PIK</strong>’s work using LPJ. E.g. inclusion of permafrost,<br />

a key influence on ecology in the boreal regions,<br />

into LPJ-DGVM led to a considerable increase in model<br />

per<strong>for</strong>mance. LPJ-DGVM representation of the hydrological<br />

cycle has been improved and successfully validated<br />

against seasonal, local- to global-scale data.<br />

First Results<br />

RECENT TERRESTRIAL CO 2 EXCHANGE<br />

LPJ-DGVM seasonal carbon exchange has been compared<br />

over regions with those derived from atmospheric<br />

inversions. The importance of such work is first to locate<br />

the main source-sink regions, important <strong>for</strong> environmental<br />

policy (e.g. Kyoto debate), and second to identify,<br />

understand and model the underlying processes sensitive<br />

to current climatic variability, giving an insight into possible<br />

future environmental changes.<br />

GREENING OF THE NORTHERN LATITUDES<br />

Using time series of climate data, the LPJ-DGVM models<br />

an advance of spring in the last two decades and an<br />

increase of vegetation abundance in the global boreal<br />

zone. This is in excellent agreement with the observed<br />

trends found independently in satellite data. The model<br />

also reproduces the impact of atmospheric aerosols from<br />

the Mount Pinatubo volcanic eruption in 1991 on vegetation<br />

productivity and phenology in northern latitudes.<br />

MODELLING OF REGIONAL FIRE PATTERNS<br />

LPJ-DGVM simulates fire disturbance taking into<br />

account multiple natural and anthropogenic causes and<br />

processes such as fire spread. A regional version of this<br />

fire model adapted to the Iberian Peninsula, successfully<br />

reproduces both the number of fires occurring and the<br />

area burnt, factors that co-determine local ecosystems.<br />

This project is partly funded by BMBF, DFG, and the EU.<br />

Goal<br />

EVITA is a sub-project of BIS. EVITA aims to describe<br />

the state of vegetation by applying the concept of thermodynamics,<br />

in particular so-called exergy, to the<br />

observed spectra of the radiation balance.<br />

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