Articles | Volume 11, issue 10
https://doi.org/10.5194/gmd-11-4339-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-11-4339-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Methods for assessment of models
| 
26 Oct 2018
Methods for assessment of models |
| 26 Oct 2018
| 26 Oct 2018
The TropD software package (v1): standardized methods for calculating tropical-width diagnostics
Hebrew University of Jerusalem, Jerusalem, Israel
Kevin M. Grise
University of Virginia, Charlottesville, VA, USA
Paul Staten
Indiana University, Bloomington, IN, USA
Isla R. Simpson
National Center for Atmospheric Research, Boulder, CO, USA
Sean M. Davis
NOAA Earth System Research Laboratory Chemical Sciences Division, Boulder, CO, USA
Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA
Nicholas A. Davis
NOAA Earth System Research Laboratory Chemical Sciences Division, Boulder, CO, USA
Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA
Darryn W. Waugh
Department of Earth and Planetary Sciences, Johns Hopkins University, Baltimore, MD, USA
Thomas Birner
Colorado State University, Fort Collins, CO, USA
currently at: Meteorologisches Institut, Ludwig-Maximilians-Universität, Munich, Germany
Alison Ming
British Antarctic Survey, Cambridge, UK
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- Mid-Latitude Jet Response to Pan-Arctic and Regional Arctic Warming in Idealized GCM G. Yang et al. 10.3390/atmos14030510
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39 citations as recorded by crossref.
- Disconnect Between Hadley Cell and Subtropical Jet Variability and Response to Increased CO2 M. Menzel et al. 10.1029/2019GL083345
- Water Resources Change in Central-Western Argentina Under the Paris Agreement Warming Targets J. Rivera et al. 10.3389/fclim.2020.587126
- Impact of Changing Winds on the Mauna Loa CO2 Seasonal Cycle in Relation to the Pacific Decadal Oscillation Y. Jin et al. 10.1029/2021JD035892
- Tropical Belt Width Proportionately More Sensitive to Aerosols Than Greenhouse Gases X. Zhao et al. 10.1029/2019GL086425
- Is Hadley Cell Expanding? T. Xian et al. 10.3390/atmos12121699
- Poleward Shift of Northern Subtropics in Winter: Time of Emergence of Zonal Versus Regional Signals R. D'Agostino et al. 10.1029/2020GL089325
- Potential impact of tropopause sharpness on the structure and strength of the general circulation L. Boljka & T. Birner 10.1038/s41612-022-00319-6
- Regional Widening of Tropical Overturning: Forced Change, Natural Variability, and Recent Trends P. Staten et al. 10.1029/2018JD030100
- Reduced Tropical Climate Land Area Under Global Warming O. Adam et al. 10.1029/2022GL102546
- Seasonal and Annual Changes of the Regional Tropical Belt in GPS-RO Measurements and Reanalysis Datasets L. Luan et al. 10.1175/JCLI-D-19-0671.1
- Investigating Tropical Versus Extratropical Influences on the Southern Hemisphere Tropical Edge in the Unified Model P. Freisen et al. 10.1029/2021JD036106
- A simple framework for likely climate projections applied to tropical width D. Baldassare & T. Reichler 10.1007/s00382-024-07335-7
- Impact of the Stratospheric Ozone on the Northern Hemisphere Surface Climate During Boreal Winter Y. Jeong et al. 10.1029/2021JD034958
- How does tropospheric VOC chemistry affect climate? An investigation of preindustrial control simulations using the Community Earth System Model version 2 N. Stanton & N. Tandon 10.5194/acp-23-9191-2023
- Varied midlatitude shortwave cloud radiative responses to Southern Hemisphere circulation shifts M. Kelleher & K. Grise 10.1002/asl.1068
- The Observed Relationship between Pacific SST Variability and Hadley Cell Extent Trends in Reanalyses M. Rollings & T. Merlis 10.1175/JCLI-D-20-0410.1
- The Hadley circulation in a changing climate P. Lionello et al. 10.1111/nyas.15114
- A phase-space consideration of changing climate-PDF L. Reimann & J. von Storch 10.1007/s00382-020-05130-8
- Breakdown of the Linear Relationship between the Southern Hemisphere Hadley Cell Edge and Jet Latitude Changes in the Last Glacial Maximum S. Kim & S. Son 10.1175/JCLI-D-19-0531.1
- Metrics of the Hadley circulation strength and associated circulation trends M. Pikovnik et al. 10.5194/wcd-3-625-2022
- On the pattern of interannual polar vortex–ozone co-variability during northern hemispheric winter F. Harzer et al. 10.5194/acp-23-10661-2023
- Recent Tropical Expansion: Natural Variability or Forced Response? K. Grise et al. 10.1175/JCLI-D-18-0444.1
- Large uncertainty in observed estimates of tropical width from the meridional stream function D. Baldassare et al. 10.5194/wcd-4-531-2023
- Hadley cell expansion in CMIP6 models K. Grise & S. Davis 10.5194/acp-20-5249-2020
- Association of the cloud radiative effect with the changes in the northern edge of Hadley circulation between the CMIP5 and CMIP6 models in boreal summer S. Gui et al. 10.1007/s00704-023-04679-8
- Improved representation of atmospheric dynamics in CMIP6 models removes climate sensitivity dependence on Hadley cell climatological extent B. De et al. 10.1002/asl.1073
- Regional Characteristics of Variability in the Northern Hemisphere Wintertime Polar Front Jet and Subtropical Jet in Observations and CMIP6 Models X. Liu et al. 10.1029/2021JD034876
- Non‐Monotonic Response of the Climate System to Abrupt CO2 Forcing I. Mitevski et al. 10.1029/2020GL090861
- Replicating the Hadley cell edge and subtropical jet latitude disconnect in idealized atmospheric models M. Menzel et al. 10.5194/wcd-5-251-2024
- Energetic constraints on the time-dependent response of the ITCZ to volcanic eruptions M. Erez & O. Adam 10.1175/JCLI-D-21-0146.1
- The Southeast Asian monsoon and El Niño–Southern Oscillation impact on the summer atmospheric circulation of East Mediterranean during 20th century based on ERA‐20C and CMIP5 simulations I. Logothetis et al. 10.1002/joc.7510
- Both differential and equatorial heating contributed to African monsoon variations during the mid-Holocene O. Adam et al. 10.1016/j.epsl.2019.06.019
- The Role of Zonally Averaged Climate Change in Contributing to Intermodel Spread in CMIP5 Predicted Local Precipitation Changes C. Garfinkel et al. 10.1175/JCLI-D-19-0232.1
- An Evaluation of the Large‐Scale Atmospheric Circulation and Its Variability in CESM2 and Other CMIP Models I. Simpson et al. 10.1029/2020JD032835
- Effects of paleogeographic changes and CO2 variability on northern mid-latitudinal temperature gradients in the Cretaceous K. Gianchandani et al. 10.1038/s41467-023-40905-7
- A Shallow Thermocline Bias in the Southern Tropical Pacific in CMIP5/6 Models Linked to Double‐ITCZ Bias M. Samuels et al. 10.1029/2021GL093818
- Mid-Latitude Jet Response to Pan-Arctic and Regional Arctic Warming in Idealized GCM G. Yang et al. 10.3390/atmos14030510
- A multivariate probabilistic framework for tracking the regional tropical edges: analysis of inter-annual variations and long-term trends X. Feng et al. 10.1088/1748-9326/ad3b23
- Determination of tropical belt widening using multiple GNSS radio occultation measurements M. Darrag et al. 10.5194/angeo-40-359-2022
3 citations as recorded by crossref.
- Regional and Seasonal Characteristics of the Recent Expansion of the Tropics K. Grise et al. 10.1175/JCLI-D-18-0060.1
- Revisiting ozone measurements as an indicator of tropical width S. Davis et al. 10.1186/s40645-018-0214-5
- Revisiting the Relationship among Metrics of Tropical Expansion D. Waugh et al. 10.1175/JCLI-D-18-0108.1
Latest update: 17 Jul 2024
Short summary
Due to incoherent methodologies, estimates of tropical width variations differ significantly across studies. Here, methods for eight commonly-used metrics of the tropical width are implemented in the Tropical-width Diagnostics (TropD) code package. The method compilation and analysis provide tools and information which help reduce the methodological component of the uncertainty associated with calculations of the tropical width.
Due to incoherent methodologies, estimates of tropical width variations differ significantly...
