Earth system models of intermediate complexity: closing the gap in the spectrum of climate system models
By M. Claussen, L. Mysak, A. Weaver, Michel Crucifix, T. Fichefet, M. Loutre, S. Weber, Joseph Alcamo, Vladimir A Alexeev, A. Berger and 9 more. 2002
589 citations recorded by the source corpus.
Subfields: Environmental Engineering, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/a7d3099e1d99953d16d93f7525d118c1da37dc4e
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Environmental Engineering
- Thomas W. Hertel
- Uris Lantz C. Baldos
- Andrea Roventini
- Jouni Raäisaänen
- David B. Lobell
- Francesco Lamperti
- Roger A. Pielke Sr.
- S. Weber
In Global and Planetary Change
- C. Bitz
- Reto Knutti
- Jouni Raäisaänen
- David B. Lobell
- A. Ganopolski
- A. Timmermann
- A. Mouchet
- J. Salas
Citations in the corpus
- Trends of Climate Change in Saudi Arabia: Implications on Water Resources (2018, background): “Few studies have reported that the free surface evaporation from wadies in Saudi Arabia could be in the range of 5–80% of water on annual basis [25,27].”
- The UVic earth system climate model: Model description, climatology, and applications to past, present and future climates (2001, result): “Our approach is complementary to that of major coupled AOGCM centres, and our model fills an important gap within the hierarchy of climate models (Claussen et al., 2001; Shackley et al., 1998).”
- Thermohaline circulation hysteresis: A model intercomparison (2005, methodology): “We will describe results of a standardized freshwater perturbation experiment conducted with eleven different models at nine scientific institutions in seven countries, as a part of the international network of Earth system models of intermediate complexity (EMICs [Claussen et al., 2002]).”
- Uncertainty Analysis of Climate Change and Policy Response (2003, unknown): “, 1999 ) , an earth system model of intermediate complexity ( Claussen , 2002 ) .”
- The faint young Sun problem (2012, background): “Notwithstanding these problems, the Archean climate was almost certainly warm enough to keep the ocean surface from freezing completely despite the low solar luminosity.”
- Transient simulation of the last glacial inception. Part I: glacial inception as a bifurcation in the climate system (2005, background): “For this reason, a new class of models - Earth system models of intermediate complexity or EMICs, (Claussen et al. 2002) - finds broad application for the study of palaeoclimates.”
- Simulating present-day climate with the INMCM4.0 coupled model of the atmospheric and oceanic general circulations (2010, methodology): “A coupled atmosphere–ocean model [10] developed at the Institute of Atmospheric Physics (IAP) of the Russian Academy of Sciences to study long�term cli� mate changes belongs to the class of the so�called models of intermediate complexity [ 11 ].”
- Climate adaptation as mitigation: the case of agricultural investments (2013, methodology): “This is analogous to the use of simplified integrated assessment models such as DICE [4], as well as intermediate complexity models in climate science [24], which reproduce the broad behavior of more complex models but sacrifice detail in order to allow a much larger number of simulations for activi”
- Description of the Earth system model of intermediate complexity LOVECLIM version 1.2 (2010, background): “1) is a three-dimensional Earth system model of intermediate complexity (EMIC, Claussen et al., 2002), i.e. its spatial resolution is coarser than that of stateof-the-art climate General Circulation Models (GCMs) and its representation of physical processes is simpler.”
- Nonlinearities, Feedbacks and Critical Thresholds within the Earth's Climate System (2004, methodology): “Structure of CLIMBER-2, an Earth System Model of Intermediate Complexity (EMIC; Claussen et al., 2002).”
- How reliable are climate models? (2007, background): “…climate models that describe the state of the climate system with at most a few tens of numbers (Harvey et al., 1997) via Earth System Models of Intermediate Complexity (EMICs) (Claussen et al., 2002) to three-dimensional global General Circulation Models (GCMs) and Regional Climate Models (RCMs).”
- Global Catastrophic Risks (2008, background): “In between there lies a range of Earth system models of intermediate complexity (EMICs) (Claussen et al., 2002; Lenton et al., 2006) which aim at resolving some range of physical processes between the global scale represented by EBMs and the more comprehensive scales represented by GCMs. EMICs are…”