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A robust increase in the eddy length scale in the simulation of future climates
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Output from the Coupled Model Intercomparison Phase 3 are analysed. It is shown that for the ‘A2’ business as usual scenario, every model exhibits an increase in the eddy length scale in the future compared with the simulation of 20th Century climate. The increase in length scale is on the order of 5% by the end of the 21st century, and the Southern Hemisphere exhibits a larger increase than the Northern Hemisphere. The inter‐model variability in the increase in the eddy length scale is correlated with the variability in the increase in dry static stability at 700 hPa. Inspection of the NCEP/NCAR reanalysis data indicates that the eddy length scale in the Southern Hemisphere may have increased in recent decades.
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“The vertical velocity still depends on RHS, but changes in this would be expected to be relatively small given modest changes in eddy kinetic energy [57] and eddy length [40].”
From Precipitation Extremes Under Climate Change (2015) · cites this paper as [40]
Citations
Cites
Atmospheric and Oceanic Fluid Dynamics: Fundamentals and Large-scale Circulation
Vallis, G. K. (2006) · Cambridge University Press eBooks · doi:10.1017/cbo9780511790447 · Cited by 1,599
Self-citationWaves and turbulence on a beta-plane
Rhines, P. B. (1975) · Journal of Fluid Mechanics · doi:10.1017/s0022112075001504 · Cited by 1,177
Research works printed but not linked: 13
- 10.1029/2006GL027504 · DOI
- 10.1175/JAS3753.1 · DOI
- Holton J., 1992, An Introduction to Dynamic Meteorology
- 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2 · DOI
- 10.1029/2006JD008087 · DOI
- 10.1175/2008JCLI2200.1 · DOI
- 10.1175/BAMS-88-9-1383 · DOI
- Meehl G. T. S., 2007, Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, 747
- 10.1175/JAS3699.1 · DOI
- 10.1175/1520-0469(1997)054<0869:GTOTFT>2.0.CO;2 · DOI
- 10.1175/1520-0485(1993)023<1346:GOMFAJ>2.0.CO;2 · DOI
- 10.1175/JAS3762.1 · DOI
- 10.1029/2005GL023684 · DOI
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“The vertical velocity still depends on RHS, but changes in this would be expected to be relatively small given modest changes in eddy kinetic energy [57] and eddy length [40].”
BackgroundThe expanding tropics: a critical assessment of the observational and modeling studies
Lucas, C., Timbal, B., & Nguyen, H. (2013) · Wiley Interdisciplinary Reviews Climate Change · doi:10.1002/wcc.251 · Cited by 268
IMDAA: High Resolution Satellite-era Reanalysis for the Indian Monsoon Region
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“• influences on eddy phase speed (Chen and Held, 2007); • influences on eddy length scales (Kidston et al., 2010; Rivière, 2011); • changes to the index of refraction for baroclinic systems (Simpson et al.”
BackgroundPhysics of Changes in Synoptic Midlatitude Temperature Variability
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“For example, if higher-order terms involving higher derivatives of the mean potential temperature need to be considered in the expansion (1), non-Gaussian statistics can arise through the terms that are nonlinear in h (Kimura and Kraichnan 1993).”
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“One possibility is that the poleward shift of the jet streams in the future climate may come from the increased eddy length scale as suggested by Kidston et al. (2010). Very recently, Kidston et al.”
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Tamarin‐Brodsky, T., & Kaspi, Y. (2017) · Nature Geoscience · doi:10.1038/s41561-017-0001-8 · Cited by 126
Garfinkel, C., Waugh, D., & Gerber, E. (2012) · Journal of Climate · doi:10.1175/jcli-d-12-00301.1 · Cited by 126
“…(2012) also conclude that changes in EHF are not consistent with the magnitude of the jet shift in their transient experiments. c. Eddy length scale Kidston et al. (2010) find that eddy length scales have increased in the SH over the past three decades, and Rivière (2011) argues that such a…”
BackgroundThe Effective Static Stability Experienced by Eddies in a Moist Atmosphere
O'Gorman, P. (2011) · Journal of the Atmospheric Sciences · doi:10.1175/2010jas3537.1 · Cited by 106
“The extratropical eddy length has increased in the Southern Hemisphere in recent decades according to reanalysis data, and also increases in simulations of global warming scenarios (Kidston et al. 2010).”
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The remote impacts of climate feedbacks on regional climate predictability
Roe, G., Feldl, N., Armour, K., Hwang, Y.-T., & Frierson, D. (2015) · Nature Geoscience · doi:10.1038/ngeo2346 · Cited by 95
Midlatitude storms in a moister world: lessons from idealized baroclinic life cycle experiments
Booth, J., Wang, S., & Polvani, L. (2012) · Climate Dynamics · doi:10.1007/s00382-012-1472-3 · Cited by 93
“CCSM: Community Climate System Model project, supported by the, Directorate for Geosciences of the National Science Foundation, and the Office of Biological and Environmental Research of the U.S. Department of Energy.”
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Barnes, E., & Hartmann, D. (2011) · doi:10.1175/jas-d-11-039.1 · Cited by 89
“We follow Vallis et al. (2004) and Barnes et al.”
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Self-citationSouthern westerlies in LGM and future (RCP4.5) climates
Chavaillaz, Y., Codron, F., & Kageyama, M. (2013) · Climate of the past · doi:10.5194/cp-9-517-2013 · Cited by 88
Is climate sensitivity related to dynamical sensitivity?
Grise, K., & Polvani, L. M. (2013) · doi:10.1002/2015jd024687 · Cited by 76
“…increases in the phase speed of baroclinic eddies [Chen and Held, 2007; Chen et al., 2008], increases in the length scale of baroclinic eddies [Kidston et al., 2010; Kidston et al., 2011], increased wave reflection on the poleward flank of the jet [Lorenz, 2014], and biases in the…”
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Tamarin, T., & Kaspi, Y. (2017) · doi:10.1002/2017gl073633 · Cited by 75
Extratropical Cyclones in Idealized Simulations of Changed Climates
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“A moderate increase of the eddy length with warming has also been found in other idealized models (Caballero and Hanley 2012) and in full GCM simulations of future climate (Kidston et al. 2010).”
BackgroundFeldstein, S., & Lee, S. (2014) · doi:10.1175/jcli-d-14-00057.1 · Cited by 69
Understanding the Dynamics of Future Changes in Extreme Precipitation Intensity
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“For example, one can compare Figure S3a multiplied by 2𝜋 with Figure 1 of Kidston et al. (2010).”
BackgroundMethodResultStorm Track Shifts under Climate Change: What Can Be Learned from Large-Scale Dry Dynamics
Mbengue, C., & Schneider, T. (2013) · doi:10.1175/jcli-d-13-00404.1 · Cited by 63
“Yet others suggest that increasing eddy length scales under global warming may play a role in storm track shifts (Kidston et al. 2010; Rivi (cid:1) ere 2011).”
BackgroundSize of the Atmospheric Blocking Events: Scaling Law and Response to Climate Change
Nabizadeh, E., Hassanzadeh, P., Yang, D., & Barnes, E. A. (2019) · Geophysical Research Letters · doi:10.1029/2019gl084863 · Cited by 86
“(6) Note that while 𝜆 is an imposed variable in the QG model, it can be readily measured in the data by computing the buoyancy frequency and tropopause height (see supporting information and Kidston et al., 2010).”
BackgroundResultInfluentialXian, T., Xia, J., Wei, W., Zhang, Z.-H., Wang, R., Wang, L.-P., & Ma, Y. (2021) · Atmosphere · doi:10.3390/atmos12121699 · Cited by 53
“Changes to the eddy length scale may also be a factor, perhaps in response to an increase in upper-tropospheric baroclinicity in the midlatitudes [19,157].”
BackgroundEddy-Driven Jet Sensitivity to Diabatic Heating in an Idealized GCM
Baker, H. S., Woollings, T., & Mbengue, C. (2017) · doi:10.1175/jcli-d-16-0864.1 · Cited by 51
Lorenz, D. (2014) · doi:10.1175/jas-d-13-0200.1 · Cited by 51
“This poleward shift is especially interesting because the direct radiativeconvective effects of rising GHG seem to project much more strongly on the strength of the midlatitude jet.”
BackgroundResultInfluentialWu, Y., Seager, R., Ting, M., Naik, N., & Shaw, T. (2012) · Journal of Climate · doi:10.1175/jcli-d-11-00284.1 · Cited by 48
“Kidston et al. (2010, 2011) found a robust increase in eddy length scale in the CMIP3–IPCC AR4 models, which is possibly caused by increased static stability in the midlatitudes.”
BackgroundMbengue, C., & Schneider, T. (2017) · Journal of the Atmospheric Sciences · doi:10.1175/jas-d-15-0267.1 · Cited by 48
“It is shown that in simulations of dry atmospheres, changes in the latitude of maximum MAPE are dominated by changes in near-surface meridional temperature gradients.”
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Ceppi, P., & Shepherd, T. G. (2017) · Journal of Climate · doi:10.1175/jcli-d-17-0189.1 · Cited by 47
“The first is associated with the fact that the basic state affects the preferred dynamical modes of variability and modes of response to radiative forcing (Ring and Plumb 2008; Sigmond and Scinocca 2010; Kidston et al. 2010; Barnes and Hartmann 2011; Simpson and Polvani 2016).”
BackgroundDelcambre, S. C., Lorenz, D., Vimont, D., & Martin, J. E. (2013) · Journal of Climate · doi:10.1175/jcli-d-12-00359.1 · Cited by 44
“In addition to the direct effects of climate change, a poleward shift of the jet streams has been simulated by climate models (Yin 2005; Johanson and Fu 2009; Lu et al. 2007; Wu et al. 2010; Lorenz and DeWeaver 2007; Kushner et al. 2001) and predicted statistically and dynamically.”
BackgroundMethodResponse of Vertical Velocities in Extratropical Precipitation Extremes to Climate Change
Li, Z., & O'Gorman, P. (2019) · Journal of Climate · doi:10.1175/jcli-d-19-0766.1 · Cited by 42
“In addition, changes in advective forcing could be better understood by relating them to changes in eddy kinetic energy (O’Gorman 2010) and changes in the horizontal length scales of the geostrophic winds (Kidston et al. 2010).”
BackgroundChanging duration and spatial extent of midlatitude precipitation extremes across different climates
Dwyer, J., & O'Gorman, P. (2017) · Geophysical Research Letters · doi:10.1002/2017gl072855 · Cited by 38
“Similarly for the comprehensive climate model projections, we find changes in zonal length of both signs depending on latitude in the CMIP5 models, but previous work has found robust increases in eddy length with warming [Kidston et al., 2010].”
BackgroundMethodResultInfluentialWu, Y., Seager, R., Shaw, T., Ting, M., & Naik, N. (2013) · Journal of Climate · doi:10.1175/jcli-d-12-00104.1 · Cited by 36
“…have been proposed to understand the tropospheric circulation shift in response to global warming such as the increase in eddy phase speed (Lu et al. 2008; Chen et al. 2008), the rise in tropopause height (Lorenz andDeWeaver 2007), and the increase in eddy length scale (Kidston et al. 2010, 2011).”
BackgroundMethodInfluentialMidlatitude Eddies, Storm-Track Diffusivity, and Poleward Moisture Transport in Warm Climates
Caballero, R., & Hanley, J. (2012) · Journal of the Atmospheric Sciences · doi:10.1175/jas-d-12-035.1 · Cited by 32
“The eddy length scale is about 2500 km in the colder runs and increases slightly with temperature, as also found in many other models (Kidston et al. 2010).”
BackgroundSingh, H. K. A., Bitz, C., Donohoe, A., Nusbaumer, J., & Noone, D. (2016) · Journal of Climate · doi:10.1175/jcli-d-16-0293.1 · Cited by 29
Chemke, R., & Yi, M. (2020) · Geophysical Research Letters · doi:10.1029/2020gl090441 · Cited by 27
“The above scale-dependent wave response might be linked to the projected increase in the eddy length scale (i.e., the scale that holds most of the energy, Kidston et al., 2010).”
BackgroundImpacts of the ENSO Lifecycle on Stratospheric Ozone and Temperature
Lin, J.-L., & Qian, T.-T. (2019) · Geophysical Research Letters · doi:10.1029/2019gl083697 · Cited by 27
“…adjustment in response to stratospheric potential vorticity anomalies (Ambaum & Hoskins, 2002; Black, 2002; Hartley et al., 1998; Hoskins et al., 1985), and (3) stratospheric influences on tropospheric baroclinic systems (e.g. Chen & Held, 2007; Kidston et al., 2010; Wittman et al., 2007).”
BackgroundRobust Expansion of Extreme Midlatitude Storms Under Global Warming
Dai, P., & Nie, J. (2022) · Geophysical Research Letters · doi:10.1029/2022gl099007 · Cited by 26
Trends in northern midlatitude atmospheric wave power from 1950 to 2099
Sussman, H. S., Raghavendra, A., Roundy, P., & Dai, A. (2020) · Climate Dynamics · doi:10.1007/s00382-020-05143-3 · Cited by 22
The Global Distribution of Atmospheric Eddy Length Scales
Barnes, E., & Hartmann, D. (2012) · doi:10.1175/jcli-d-11-00331.1 · Cited by 18
“Kidston et al. (2010) demonstrated that the Coupled Model Intercomparison Project phase 3 (CMIP3) general circulation models (Meehl et al. 2007) exhibit a robust increase in zonal eddy length scale in future climates, and they suggest that this increase contributes to the predicted poleward…”
BackgroundMethodTropical cyclone size is strongly limited by the Rhines scale: experiments with a barotropic model
Lu, K., & Chavas, D. (2021) · Journal of the Atmospheric Sciences · doi:10.1175/jas-d-21-0224.1 · Cited by 14
“…calculated using a single characteristic turbulent velocity, usually defined as the root-mean-square velocity (e.g., Sukoriansky et al. 2006; Kidston et al. 2010), or even a single characteristic velocity scale for a TC (an outer circulation velocity scale Uβ in CR19; a collective velocity…”
MethodSuppression of Baroclinic Eddies by Strong Jets
Hadas, O., & Kaspi, Y. (2021) · Journal of the Atmospheric Sciences · doi:10.1175/jas-d-20-0289.1 · Cited by 11
Strong Influence of Eddy Length on Boreal Summertime Extreme Precipitation Projections
Tandon, N., Nie, J., & Zhang, X.-B. (2018) · Geophysical Research Letters · doi:10.1029/2018gl079327 · Cited by 11
“As shown in T2018, this technique produces eddy length values that are quantitatively comparable to those obtained using Fourier transform techniques (Barnes & Hartmann, 2012; Frierson et al., 2006; Kidston et al., 2010).”
BackgroundMethodSchemm, S., Papritz, L., & Rivière, G. (2022) · Weather and Climate Dynamics · doi:10.5194/wcd-2022-3 · Cited by 10
The effects of increasing humidity on heat transport by extratropical waves
Geen, R., Czaja, A., & Haigh, J. (2016) · doi:10.1002/2016gl070214 · Cited by 10
Albern, N., Voigt, A., Thompson, D. W., & Pinto, J. (2020) · Journal of Climate · doi:10.1175/jcli-d-20-0073.1 · Cited by 9
Atmospheric energy transfer response to global warming
Chemke, R. (2017) · Quarterly Journal of the Royal Meteorological Society · doi:10.1002/qj.3086 · Cited by 7
“O’Gorman, 2011) in warm climates, which may be due to an increase in static stability (Kidston et al., 2010), tropopause height (O’Gorman, 2011) or upper-level baroclinicity (Rivière, 2011), may affect the strength of the inverse and forward energy cascades.”
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Soldatenko, S., & Karlin, L. (2014) · doi:10.4236/epe.2014.611032 · Cited by 5
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Palipane, E., Lu, J., Staten, P., Chen, G., & Schneider, E. (2016) · Climate Dynamics · doi:10.1007/s00382-016-3092-9 · Cited by 5
“CAM4 is the version of the community atmospheric model used for the CMIP5 project (Taylor et al. 2012) by NCAR and represents a significant improvement from the earlier version, while CM2.”
BackgroundLeung, M. Y., Wang, D., Zhou, W., Zhang, Y., & Wang, L. (2022) · Geophysical Research Letters · doi:10.1029/2022gl098297 · Cited by 4
A new understanding of the causes of future change in El Niño teleconnection
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Mpanza, M. A. T., & Tandon, N. (2022) · Climate Dynamics · doi:10.1007/s00382-022-06268-3 · Cited by 3
“To some extent, these mechanisms are related because eddy length depends on vertical stability, and eddy length is expected to change as a result of long-term changes in vertical stability (Kidston et al. 2010; Tandon et al. 2018b).”
BackgroundStorm Track Response to Perturbations in Climate
Mbengue, C. (2015) · doi:10.7907/z9ft8j05 · Cited by 3
Amplifying Variability of the Southern Annular Mode in the Past and Future
Ma, D., Zhang, Y., & Nie, J. (2026) · Geophysical Research Letters · doi:10.1029/2025gl119214 · Cited by 2
“Possible contributors include changes in the characteristic wavelength of eddies, which can modulate the eddy‐jet feedback strength (Dai and Nie, 2020; Kidston et al., 2010), and biases in the models' climatological states that affect baroclinic instability and eddy dynamics (Chemke et al., 2022).”
Mpanza, T., & Tandon, N. (2021) · doi:10.21203/rs.3.rs-462492/v1
“…because eddy length depends on vertical stability, and eddy length is expected108 to change as a result of long-term changes in vertical stability (Kidston et al, 2010;109 Tandon et al, 2018b).110 Despite the valuable insights gained from GCMs, understanding regional pro-111 cesses in GCMs is…”
BackgroundMidlatitude Storm Track Response to Increased Greenhouse Warming
Wu, Y. (2012) · doi:10.7916/d80z7993
“…possibility of the rising tropospheric static stability that shifts the Hadley Cell, the baroclinic instability zone and thus the midlatitude eddies poleward; Kidston et al. (2010) and Kidston et al. (2011) argued that the increase in eddy length scale can move the surface westerlies poleward.”
Background
Metadata
- Authors
- Kidston, J., Dean, S. M., Renwick, J. A., & Vallis, G. K.
- Affiliations
- NOAA Geophysical Fluid Dynamics Laboratory (US)
- National Institute of Water and Atmospheric Research (NZ)
- Venue
- Geophysical Research Letters
- Publisher
- American Geophysical Union (AGU)
- Published
- 2010-02
- Volume
- 37
- Issue
- 3
- ISSN
- 0094-8276 (ISSN-L)
- 1944-8007
- OpenAlex
- W1707753894
- Cited by
- 70
- References
- 0
- Citations by year
- 2026: 1 · 2024: 3 · 2023: 1 · 2022: 8 · 2021: 5 · 2020: 4 · 2019: 3 · 2018: 2 · 2017: 6 · 2016: 5 · 2015: 5 · 2014: 7 · 2013: 4 · 2012: 8
- FWCI
- 5.76
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Geophysical Research Letters (publishedVersion)
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Meteorological Phenomena and Simulations
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Keywords
- eddy length scale, future climate change, A2 emission scenario, Southern Hemisphere, Northern Hemisphere, inter-model variability, atmospheric eddies, climate change projections
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