Atmosphere‐ocean thermal coupling in the North Atlantic: A positive feedback

By M. Watanabe, M. Kimoto. 2000

550 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/43b6f0c3ccd9a79f2b23f6f2ae055c8997eae45b

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. H. Annamalai
2. K. Sperber
3. F. Jin
4. Chunzai Wang
5. Masahiro Watanabe
6. B. Mapes
7. Sang‐Ki Lee
8. Shang-Ping Xie

In Global and Planetary Change

1. H. Annamalai
2. K. Sperber
3. F. Jin
4. Masahiro Watanabe
5. Shang-Ping Xie
6. Chunzai Wang
7. B. Mapes
8. Sang‐Ki Lee

In Oceanography

1. F. Jin
2. K. Sperber
3. H. Annamalai
4. Masahiro Watanabe
5. Chunzai Wang
6. Sang‐Ki Lee
7. B. Mapes
8. Shang-Ping Xie

Citations in the corpus

• Analysis on the Dynamics of a Wave-like Teleconnection Pattern along the Summertime Asian Jet Based on a Reanalysis Dataset and Climate Model Simulations (2009, methodology): “The model is the dry version of the LBM developed by Watanabe and Kimoto (2000, 2001), with horizontal resolution of T42 and 20 vertical levels on the s coordinate.”
• Regional Heat Sources and the Active and Break Phases of Boreal Summer Intraseasonal (30–50 Day) Variability* (2005, methodology): “The model used here has been explained in detail by Watanabe and Kimoto (2000, 2001).”
• Influence of the Gulf Stream on the Barents Sea ice retreat and Eurasian coldness during early winter (2014, methodology): “A LBM, developed by Watanabe and Kimoto (2000), was used to examine steady atmospheric response to a heating anomaly over targeted areas (e.g., Barents Sea).”
• Sea surface temperature variability: patterns and mechanisms. (2010, background): “with the North Atlantic tripole are primarily forced by the atmosphere, there is some evidence for a weak feedback upon the NAO (Watanabe and Kimoto, 2000; Czaja and Frankignoul, 2002).”
• Indian Ocean Dipole Response to Global Warming: Analysis of Ocean–Atmospheric Feedbacks in a Coupled Model* (2009, methodology): “A detailed description of the linear model may be found in Watanabe and Kimoto (2000).”
• Different mechanisms for the extremely hot central-eastern China in July–August 2022 from a Eurasian large-scale circulation perspective (2023, methodology): “We also successfully reproduced similar teleconnection in July 2022 forced by the observed NWSA anomalous heating in a linear baroclinic model (LBM;Watanabe and Kimoto 2000) (figure not shown).”
• The Growth and Triggering Mechanisms of the PNA : A MJO-PNA Coherence (2008, background): “The LBM consists of primitive equations exactly linearized about a basic state (see Watanabe and Kimoto 2000, 2001, for mathematical expressions).”
• Observed Associations Among Storm Tracks, Jet Streams and Midlatitude Oceanic Fronts (2013, background): “Several experiments, however, in each of which an AGCM is coupled thermally with a slab ocean mixed layer model [Lau and Nath, 1996, 2001; Watanabe and Kimoto, 2000] showed that midlatitude SSTAs can reinforce atmospheric anomalies that have driven them.”
• A Simple Atmospheric Model of the Local and Teleconnection Responses to Tropical Heating Anomalies (2009, methodology): “Perhaps the closest relative of the current model is the multilevel linear baroclinic model (LBM) used by Hoskins and Simmons (1975) and others (e.g., Webster 1981; Kasahara and da Silva Dias 1986; Branstator 1990; Ting and Held 1990; Jin and Hoskins 1995; Watanabe and Kimoto 2000; Watanabe and Jin ”
• A Moist Linear Baroclinic Model: Coupled Dynamical–Convective Response to El Niño (2003, methodology): “The LBM used in this study is based on primitive equations exactly linearized about a basic state (see Watanabe and Kimoto 2000, 2001, for mathematical expressions ).”