The NCEP/NCAR re-analyses data as well as ensemble integrations with an atmospheric GCM indicate ...
Which physical processes effectively determine the stability regime of the Atlantic meridional ov...
We investigate the role of the ocean feedback on the climate response to insolation forcing durin...
This chapter examines the Daisymodel's steady state solution with emphasis on the mechanisms that...
In this paper we examine the orbital signal in Earth's climate with a coupled model of intermedia...
Synthetic glacier length records are generated for the Holocene epoch using a process-based glaci...
We propose a new perspective on the hierarchy of climate models which goes beyond the "classical"...
The steady state solution of the Daisyworld model of Watson and Lovelock (1983) is examined in de...
In a transient simulation of the Holocene climate with ECBilt orbital forcing induces a quasi-lin...
The spatio-temporal structure of low-frequency temperature variability, as reflected in a paleo n...
The seasonality of low-frequency temperature variability is studied by application of multichanne...