Spatial planning of a climate adaptation zone for wetland ecosystems
In a publication in Landscape Ecology we present a spatial planning approach for the implementation of adaptation measures to climate change in conservation planning for ecological networks…
This document describes the requirements and guidelines for the software of the IMAGE system. The motivation for this report was a substantial restructuring of the source code for IMAGE version 2.5…
The climate subsystem in IMAGE updated to MAGICC 6.0
Technical background report on the upgrade of the simple climate model MAGICC within the IMAGE model ("Integrated Model to Assess the Global Environment") of PBL.
This user manual contains the basic information for running the simulation model IMAGE ("Integrated Model to Assess the Global Environment") of PBL. The motivation for this report was a substantial…
The HYDE 3.1 spatially explicit database of human-induced global land-use change over the past 12,000 years
This paper presents a tool for long term global change studies; it is an update of the History Database of the Global Environment (HYDE) with estimates of some of the underlying demographic and…
Anthropogenic transformation of the biomes, 1700 to 2000
The aim was to map and characterize anthropogenic transformation of the terrestrial biosphere before and during the Industrial Revolution, from 1700 to 2000.
Options to accelerate ozone recovery: ozone and climate benefits
Hypothetical reductions in future emissions of ozone-depleting substances (ODSs) and N 2 O are evaluated in terms of effects on equivalent effective stratospheric chlorine (EESC), globally-averaged…
Phosphorus demand for the 1970–2100 period: A scenario analysis of resource depletion
The phosphorus (P) cycle has been significantly altered by human activities. For this paper, we explored the sustainability of current P flows in terms of resource depletion and the ultimate fate of…
Exploring IMAGE model scenarios that keep greenhouse gas radiative forcing below 3 W/m2 in 2100
A high probability of limiting temperature increase to 2 °C requires a radiative forcing below 3 W/m², around the end of this century, according to current knowledge. This paper identifies conditions…
Dealing with surplus emissions in the climate negotiations after Copenhagen: What are the options for compromise?
Our analysis suggests that maximal revenues for surplus-holding countries arise by releasing only a limited amount of surplus credits to the market. The institutionalisation of this effect could be a…
Planbureau voor de Leefomgeving
