Here we present Late Miocene (~11-7 Ma) model boundary conditions used by Knorr et al. [2011] in two files (Paleogeography.nc and Surface_conditions.nc). These boundary conditions relate to Figure 1 in the corresponding study. The file Paleogeography.nc (0.5°x 0.5° resolution) contains the orography (positive values and zero) and bathymetry (negative values). The file Surface_conditions.nc contains land surface conditions. Besides the glacier mask these surface conditions (3.75°x 3.75° resolution) contain the vegetation distribution that is represented by specifying different land surface parameters including, surface albedo, surface roughness length, field capacity of soil, forest ratio, leaf area index, fractional vegetation cover, and ...
peer reviewedThe CARAIB (CARbon Assimilation In the Biosphere) model is used to study the vegetation...
The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative to today. Continent...
There is an increasing need to understand the pre-Quaternary warm climates, how climate–vegetation i...
General circulation models (GCMs) are useful tools for investigating the characteristics and dynami...
peer reviewedThe Miocene is a relatively recent epoch of the Earth's history with warmer climate tha...
The Middle Miocene Climate Transition was characterized by major Antarctic ice sheet expansion and ...
The late Miocene palaeorecord provides evidence for a warmer and wetter climate than that of today, ...
The Middle Miocene Climate Transition was characterized by major Antarctic ice-sheet expansion and g...
The late Miocene palaeorecord provides evidence for a warmer and wetter climate than that of today, ...
The Late Miocene (∼11.6–5.3 Ma) palaeorecord provides evidence for a warmer and wetter climate than ...
In a long-term climatic cooling trend, the Middle Miocene represents one of the last warm periods of...
There is an increasing need to understand the pre-Quaternary warm climates, how climate–vegetation i...
The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative to today. Continent...
Supporting Information for Simulating Miocene warmth: insights from an opportunistic Multi-Model ens...
The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative to today. Continent...
peer reviewedThe CARAIB (CARbon Assimilation In the Biosphere) model is used to study the vegetation...
The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative to today. Continent...
There is an increasing need to understand the pre-Quaternary warm climates, how climate–vegetation i...
General circulation models (GCMs) are useful tools for investigating the characteristics and dynami...
peer reviewedThe Miocene is a relatively recent epoch of the Earth's history with warmer climate tha...
The Middle Miocene Climate Transition was characterized by major Antarctic ice sheet expansion and ...
The late Miocene palaeorecord provides evidence for a warmer and wetter climate than that of today, ...
The Middle Miocene Climate Transition was characterized by major Antarctic ice-sheet expansion and g...
The late Miocene palaeorecord provides evidence for a warmer and wetter climate than that of today, ...
The Late Miocene (∼11.6–5.3 Ma) palaeorecord provides evidence for a warmer and wetter climate than ...
In a long-term climatic cooling trend, the Middle Miocene represents one of the last warm periods of...
There is an increasing need to understand the pre-Quaternary warm climates, how climate–vegetation i...
The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative to today. Continent...
Supporting Information for Simulating Miocene warmth: insights from an opportunistic Multi-Model ens...
The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative to today. Continent...
peer reviewedThe CARAIB (CARbon Assimilation In the Biosphere) model is used to study the vegetation...
The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative to today. Continent...
There is an increasing need to understand the pre-Quaternary warm climates, how climate–vegetation i...