arxiv: 2604.04429 · v1 · submitted 2026-04-06 · ⚛️ physics.ao-ph

Recognition: 2 theorem links

· Lean Theorem

Future Amplification of Moist Weather Extremes in the Midlatitudes

Funing Li, Talia Tamarin-Brodsky

Pith reviewed 2026-05-10 20:19 UTC · model grok-4.3

classification ⚛️ physics.ao-ph

keywords moist heatwavesconvective stormsmidlatitudeslow-level inversionsorographic heatingcompound extremesclimate change

0 comments

The pith

Amplified warming from western highlands strengthens downstream low-level inversions to intensify midlatitude moist heat and convection extremes.

A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.

The paper demonstrates that moist heatwaves and convective storms will become more intense in the midlatitudes under future climate conditions. It identifies low-level atmospheric inversions as the key constraint on these extremes, with warming over highlands being advected eastward by westerlies to enhance the inversions. This process raises the possible maximum values for both moist heat and convection activity. Readers should care because it explains the emergence of specific hotspots for compound risks in areas like eastern North America and northeastern Asia.

Core claim

The intensification of concurrent moist heat and convection extremes in the midlatitudes is tightly constrained by changes in low-level atmospheric inversions. Amplified warming over western highlands is transported downstream by prevailing westerlies, strengthening low-level thermal inversions and raising the attainable maxima of moist heat and convection. Targeted model experiments confirm the critical role of orographically elevated heating in driving these extremes.

What carries the argument

Low-level thermal inversions that are strengthened by the downstream advection of orographic warming, which in turn sets higher limits on moist heat and convective activity.

If this is right

Hotspots for compound extremes will develop in midlatitude regions east of major highlands.
Changes in inversion strength will directly control future increases in moist heatwave intensity and storm severity.
The role of orography in climate change impacts on weather extremes is highlighted as essential for accurate projections.

Where Pith is reading between the lines

These are editorial extensions of the paper, not claims the author makes directly.

This suggests that global climate models need to accurately represent orographic heating to capture midlatitude extreme risks.
Similar inversion-based amplification might occur in other parts of the world with comparable topography and wind patterns.
Interactions between this mechanism and shifts in large-scale circulation remain to be explored in detail.

Load-bearing premise

The targeted model experiments isolate the causal effect of orographic heating without confounding influences from other climate changes like circulation shifts or moisture changes.

What would settle it

Running climate model simulations without elevated heating over western highlands and observing whether the projected amplification of midlatitude moist extremes disappears or persists at similar levels.

read the original abstract

Moist heatwaves and convective storms frequently co-occur, posing compound risks. Although historically concentrated in the tropics, these moist weather extremes are projected to intensify substantially towards the midlatitudes, with regions downstream of major highland terrains, including northeastern Asia and eastern North America, emerging as hotspots of future change. Yet their physical drivers remain uncertain. Here we show that the intensification of concurrent moist heat and convection extremes in the midlatitudes is tightly constrained by changes in low-level atmospheric inversions. Specifically, we find that amplified warming over western highlands is transported downstream by prevailing westerlies, strengthening low-level thermal inversions and raising the attainable maxima of moist heat and convection. Targeted model experiments confirm the critical role of orographically elevated heating in driving these extremes. Our results reveal a mechanistic pathway for compound extremes and highlight low-level inversions as a key factor for emerging midlatitude risks of moist heat and severe weather under climate change.

Editorial analysis

A structured set of objections, weighed in public.

Desk editor's note, referee report, simulated authors' rebuttal, and a circularity audit. Tearing a paper down is the easy half of reading it; the pith above is the substance, this is the friction.

Desk Editor's Note private letter to a colleague

The paper gives a mechanistic story for midlatitude moist extremes via orographic warming advected by westerlies to strengthen inversions, but the model experiments may not cleanly isolate that pathway.

read the letter

The core claim is that future amplification of concurrent moist heat and convection in the midlatitudes comes from amplified highland warming being carried downstream by westerlies, which then tightens low-level inversions and raises the ceiling on those extremes. This targets hotspots like eastern North America and northeastern Asia and offers a physical reason for the poleward shift that earlier work left open.

Referee Report

1 major / 0 minor

Summary. The paper claims that future intensification of concurrent moist heat and convection extremes in the midlatitudes is tightly constrained by changes in low-level atmospheric inversions. Amplified warming over western highlands is advected downstream by prevailing westerlies, strengthening these inversions and raising attainable maxima for moist heat and convection extremes. Targeted model experiments are used to confirm the critical role of orographic heating in driving these changes, with hotspots identified in regions such as northeastern Asia and eastern North America.

Significance. If the proposed mechanism and experimental isolation hold, the work would provide a physically grounded explanation for the projected shift of compound moist extremes into the midlatitudes, identifying low-level inversions as a key controlling factor. This could inform improved risk assessment and modeling of severe weather in populated downstream regions under climate change.

major comments (1)

[Abstract (targeted model experiments description)] The central causal claim requires that the targeted model experiments isolate the effect of orographic heating from concurrent changes in circulation, moisture advection, or boundary-layer dynamics. The abstract states that these experiments 'confirm the critical role,' but without details on the protocol (e.g., nudging of large-scale flow, fixed SSTs, prescribed heating anomalies, or controls on moisture convergence), it remains possible that inversion changes arise from altered westerlies or turbulence rather than the proposed thermal-advection pathway. This isolation step is load-bearing for the attribution.

Simulated Author's Rebuttal

1 responses · 0 unresolved

We thank the referee for their constructive review and for identifying the need to strengthen the description of our targeted model experiments. We have revised the manuscript to address this point directly.

read point-by-point responses

Referee: [Abstract (targeted model experiments description)] The central causal claim requires that the targeted model experiments isolate the effect of orographic heating from concurrent changes in circulation, moisture advection, or boundary-layer dynamics. The abstract states that these experiments 'confirm the critical role,' but without details on the protocol (e.g., nudging of large-scale flow, fixed SSTs, prescribed heating anomalies, or controls on moisture convergence), it remains possible that inversion changes arise from altered westerlies or turbulence rather than the proposed thermal-advection pathway. This isolation step is load-bearing for the attribution.

Authors: We agree that the abstract's brevity leaves the experimental isolation insufficiently explicit. In the revised manuscript we have expanded the abstract to state that the targeted experiments apply prescribed orographic heating anomalies over western highlands while holding SSTs fixed and using spectral nudging to constrain large-scale circulation; moisture convergence and boundary-layer processes are permitted to respond dynamically. The full protocol, including verification that inversion changes are driven by downstream thermal advection rather than circulation or turbulence adjustments, is detailed in Section 4 with supporting sensitivity tests. These design choices directly isolate the proposed pathway and thereby support the causal attribution. revision: yes

Circularity Check

0 steps flagged

No circularity: derivation rests on independent model experiments

full rationale

The paper's central claim—that amplified highland warming is advected downstream to strengthen low-level inversions and thereby raise attainable maxima for moist heat and convection extremes—is supported by targeted model experiments that isolate the orographic heating role. No equations, parameter fits, or self-definitions are shown that would make any prediction equivalent to its inputs by construction. The mechanism is physically motivated by westerly transport and verified externally via simulations rather than reduced to a renaming, ansatz, or self-citation chain. The derivation is therefore self-contained against external benchmarks.

Axiom & Free-Parameter Ledger

0 free parameters · 1 axioms · 0 invented entities

The abstract invokes standard atmospheric dynamics without introducing new entities or explicitly fitted parameters. The core transport assumption is treated as given from prior knowledge.

axioms (1)

domain assumption Prevailing westerlies transport amplified warming from western highlands downstream to strengthen low-level inversions
This physical transport step is the load-bearing link in the proposed mechanism and is not derived within the paper.

pith-pipeline@v0.9.0 · 5460 in / 1273 out tokens · 44281 ms · 2026-05-10T20:19:45.057352+00:00 · methodology

discussion (0)

Lean theorems connected to this paper

Citations machine-checked in the Pith Canon. Every link opens the source theorem in the public Lean library.

IndisputableMonolith/Cost/FunctionalEquation.lean washburn_uniqueness_aczel unclear
the intensification of concurrent moist heat and convection extremes in the midlatitudes is tightly constrained by changes in low-level atmospheric inversions... amplified warming over western highlands is transported downstream by prevailing westerlies, strengthening low-level thermal inversions
IndisputableMonolith/Foundation/AlphaCoordinateFixation.lean alpha_pin_under_high_calibration unclear
Targeted model experiments confirm the critical role of orographically elevated heating in driving these extremes

Reference graph

Works this paper leans on

138 extracted references · 8 canonical work pages

[1]

Accordingly, we also analyze CAPE at the time of annual maximum MSE𝑠 (i.e., critical CAPE, denoted as CAPE𝑐)

scaled by a factor of𝛼=0.22 (see (58) for detailed derivations and discussions). Accordingly, we also analyze CAPE at the time of annual maximum MSE𝑠 (i.e., critical CAPE, denoted as CAPE𝑐). CAPE𝑐 has been shown to largely coincide with the annual maximum CAPE over midlatitude continents (58). Consequently, future changes in CAPE𝑐 reflect changes in the i...
[2]

(122), MRI-ESM2-0 (r1i1p1f1, 160×320, 80) (123), MIROC6 (r1i1p1f1, 128×256, 81) (124), MIROC-ES2L (r1i1p1f2, 64×128, 40) (125), and CanESM5 (r1i1p2f1, 64×128, 49) (126). For each model, we compare the period of 1980–2009 from the historical run with the period of 2065–2094 from a high-emission future run (ssp585), in which the radiative forcing increases ...

1980
[3]

S1), the midlat- itude mean biases are relatively small in the selected models but substantially larger, especially for CAPE𝑐, in the remaining five models (Supplementary Fig

Although all models exhibit biases in annual maximum MSE𝑠 and the associated convective instability (CAPE𝑐) and low-level energy inversion (MSE∗ 𝑚𝑎𝑥 ) (Supplementary Fig. S1), the midlat- itude mean biases are relatively small in the selected models but substantially larger, especially for CAPE𝑐, in the remaining five models (Supplementary Fig. S2𝐴). In a...

1979
[4]

R. E. Morss, O. V. Wilhelmi, G. A. Meehl, L. Dilling, Improving societal outcomes of extreme weather in a changing climate: an integrated perspective.Annual Review of Environment and Resources36(1), 1–25 (2011)

2011
[5]

C. C. Ummenhofer, G. A. Meehl, Extreme weather and climate events with ecological rel- evance: a review.Philosophical Transactions of the Royal Society B: Biological Sciences 372(1723), 20160135 (2017)

2017
[6]

S. C. Sherwood, M. Huber, An adaptability limit to climate change due to heat stress.Pro- ceedings of the National Academy of Sciences107(21), 9552–9555 (2010)

2010
[7]

J. W. Baldwin,et al., Humidity’s role in heat-related health outcomes: a heated debate. Environmental health perspectives131(5), 055001 (2023)

2023
[8]

Stevens, Atmospheric moist convection.Annu

B. Stevens, Atmospheric moist convection.Annu. Rev. Earth Planet. Sci.33(1), 605–643 (2005)

2005
[9]

J. Bao, B. Stevens, L. Kluft, C. Muller, Intensification of daily tropical precipitation extremes from more organized convection.Science Advances10(8), eadj6801 (2024)

2024
[10]

Coumou, S

D. Coumou, S. Rahmstorf, A decade of weather extremes.Nature climate change2(7), 491–496 (2012)

2012
[11]

Matthews, Humid heat and climate change.Progress in Physical Geography: Earth and Environment42(3), 391–405 (2018)

T. Matthews, Humid heat and climate change.Progress in Physical Geography: Earth and Environment42(3), 391–405 (2018)

2018
[12]

E. J. Zipser, C. Liu, Extreme convection vs. extreme rainfall: A global view.Current Climate Change Reports7(4), 121–130 (2021)

2021
[13]

S. Kang, E. A. Eltahir, North China Plain threatened by deadly heatwaves due to climate change and irrigation.Nature communications9(1), 2894 (2018)

2018
[14]

Zhang,et al., Moisture from US Corn Belt fuels more intense convective storms.Commu- nications Earth & Environment(2025)

Z. Zhang,et al., Moisture from US Corn Belt fuels more intense convective storms.Commu- nications Earth & Environment(2025). 23

2025
[15]

Q. Kong, M. Huber, Regimes of Soil Moisture–Wet-Bulb Temperature Coupling with Rele- vance to Moist Heat Stress.Journal of Climate36(22), 7925–7942 (2023)

2023
[16]

F. Li, D. R. Chavas, B. Medeiros, K. A. Reed, K. L. Rasmussen, Upstream surface roughness and terrain are strong drivers of contrast in tornado potential between North and South America.Proceedings of the National Academy of Sciences121(26), e2315425121 (2024)

2024
[17]

Tamarin-Brodsky, K

T. Tamarin-Brodsky, K. Hodges, B. J. Hoskins, T. G. Shepherd, Changes in Northern Hemi- sphere temperature variability shaped by regional warming patterns.Nature Geoscience13(6), 414–421 (2020)

2020
[18]

Jiang, D

Q. Jiang, D. T. Dawson II, F. Li, D. R. Chavas, Classifying synoptic patterns driving tornadic storms and associated spatial trends in the United States.npj Climate and Atmospheric Science 8(1), 7 (2025)

2025
[19]

Raymond, T

C. Raymond, T. Matthews, R. M. Horton, The emergence of heat and humidity too severe for human tolerance.Science Advances6(19), eaaw1838 (2020)

2020
[20]

C. D. Rogers,et al., Recent increases in exposure to extreme humid-heat events dispropor- tionately affect populated regions.Geophysical Research Letters48(19), e2021GL094183 (2021)

2021
[21]

D. I. Domeisen,et al., Prediction and projection of heatwaves.Nature Reviews Earth & Environment4(1), 36–50 (2023)

2023
[22]

Barriopedro, R

D. Barriopedro, R. Garc ´ıa-Herrera, C. Ord ´onez, D. G. Miralles, S. Salcedo-Sanz, Heat waves: Physical understanding and scientific challenges.Reviews of Geophysics61(2), e2022RG000780 (2023)

2023
[23]

D. M. Romps, Y.-C. Lu, Chronically underestimated: a reassessment of US heat waves using the extended heat index.Environmental Research Letters17(9), 094017 (2022)

2022
[24]

J. R. Lanzante, A new heat stress index for climate change assessment.Bulletin of the American Meteorological Society105(12), E2482–E2495 (2024). 24

2024
[25]

W. R. Xu, K. W. Dixon, N. Zenes, D. Adams-Smith, Sometimes missing the heat: the risk of underestimating extreme heat days with daily maximum heat index approximation.Interna- tional Journal of Biometeorologypp. 1–15 (2025)

2025
[26]

E. J. Zipser, D. J. Cecil, C. Liu, S. W. Nesbitt, D. P. Yorty, Where are the most intense thunderstorms on Earth?Bulletin of the American Meteorological Society87(8), 1057–1072 (2006)

2006
[27]

H. E. Brooks, J. W. Lee, J. P. Craven, The spatial distribution of severe thunderstorm and tornado environments from global reanalysis data.Atmospheric Research67, 79–94 (2003), doi:https://doi.org/10.1016/S0169-8095(03)00045-0

work page doi:10.1016/s0169-8095(03)00045-0 2003
[28]

A. F. Prein, Thunderstorm straight line winds intensify with climate change.Nature Climate Change13(12), 1353–1359 (2023)

2023
[29]

B. H. Tang, V. A. Gensini, C. R. Homeyer, Trends in United States large hail environments and observations.NPJ Climate and Atmospheric Science2(1), 45 (2019)

2019
[30]

N. N. C. for Environmental Information (NCEI), U.S. Billion-Dollar Weather and Cli- mate Disasters (2025), doi:10.25921/stkw-7w73,https://www.ncei.noaa.gov/access/ billions/

work page doi:10.25921/stkw-7w73 2025
[31]

Sauter,et al., Compound extreme hourly rainfall preconditioned by heatwaves most likely in the mid-latitudes.Weather and Climate Extremes40, 100563 (2023)

C. Sauter,et al., Compound extreme hourly rainfall preconditioned by heatwaves most likely in the mid-latitudes.Weather and Climate Extremes40, 100563 (2023)

2023
[32]

Treppiedi, G

D. Treppiedi, G. Villarini, L. V. Noto, Climate change exacerbates the compounding of heat stress and flooding in the mid-latitudes.International Journal of Climatology44(7), 2283–2296 (2024)

2024
[33]

Sauter, C

C. Sauter, C. J. White, H. J. Fowler, S. Westra, Temporally compounding heatwave–heavy rainfall events in Australia.International Journal of Climatology43(2), 1050–1061 (2023)

2023
[34]

Z. Xu, Y. Zhang, G. Bl¨oschl, S. Piao, Mega forest fires intensify flood magnitudes in southeast Australia.Geophysical Research Letters50(12), e2023GL103812 (2023). 25

2023
[35]

Ganguli, B

P. Ganguli, B. Merz, Increasing probability of extreme rainfall preconditioned by humid heatwaves in global coastal megacities.npj Climate and Atmospheric Science8(1), 144 (2025)

2025
[36]

Sauter, J

C. Sauter, J. L. Catto, H. J. Fowler, S. Westra, C. J. White, Compounding Heatwave-Extreme Rainfall Events Driven by Fronts, High Moisture, and Atmospheric Instability.Journal of Geophysical Research: Atmospheres128(21), e2023JD038761 (2023)

2023
[37]

Vyshkvarkova, O

E. Vyshkvarkova, O. Sukhonos, Compound extremes of air temperature and precipitation in Eastern Europe.Climate10(9), 133 (2022)

2022
[38]

J. You, S. Wang, Higher probability of occurrence of hotter and shorter heat waves followed by heavy rainfall.Geophysical Research Letters48(17), e2021GL094831 (2021)

2021
[39]

Li,et al., Substantial increase in heavy precipitation events preceded by moist heatwaves over China during 1961–2019.Frontiers in Environmental Science10, 951392 (2022)

C. Li,et al., Substantial increase in heavy precipitation events preceded by moist heatwaves over China during 1961–2019.Frontiers in Environmental Science10, 951392 (2022)

1961
[40]

Miao,et al., Unveiling the dynamics of sequential extreme precipitation-heatwave com- pounds in China.npj Climate and Atmospheric Science7(1), 67 (2024)

L. Miao,et al., Unveiling the dynamics of sequential extreme precipitation-heatwave com- pounds in China.npj Climate and Atmospheric Science7(1), 67 (2024)

2024
[41]

Zhang, G

W. Zhang, G. Villarini, Deadly compound heat stress-flooding hazard across the Central United States.Geophysical Research Letters47(15), e2020GL089185 (2020)

2020
[42]

Hao,et al., Evaluating the effects of heatwave events on hydrological processes in the contiguous United States (2003–2022).Journal of Hydrology637, 131368 (2024)

Y. Hao,et al., Evaluating the effects of heatwave events on hydrological processes in the contiguous United States (2003–2022).Journal of Hydrology637, 131368 (2024)

2003
[43]

Zhou,et al., Global increase in future compound heat stress-heavy precipitation hazards and associated socio-ecosystem risks.Npj Climate and Atmospheric Science7(1), 33 (2024)

Z. Zhou,et al., Global increase in future compound heat stress-heavy precipitation hazards and associated socio-ecosystem risks.Npj Climate and Atmospheric Science7(1), 33 (2024)

2024
[44]

J. Liu, J. Chen, J. Yin, A. D. King, Time of emergence of record-shattering compound heatwave-extreme precipitation events and their socio-economic exposures.Geophysical Re- search Letters52(16), e2025GL116884 (2025)

2025
[45]

Russo, J

S. Russo, J. Sillmann, A. Sterl, Humid heat waves at different warming levels.Scientific reports7(1), 7477 (2017). 26

2017
[46]

Lepore, R

C. Lepore, R. Abernathey, N. Henderson, J. T. Allen, M. K. Tippett, Future Global Convective Environments in CMIP6 Models.Earth’s Future9(12), e2021EF002277 (2021)

2021
[47]

Jin,et al., Global escalation of more frequent and intense compound heatwave-extreme precipitation events.EGUsphere2025, 1–30 (2025)

H. Jin,et al., Global escalation of more frequent and intense compound heatwave-extreme precipitation events.EGUsphere2025, 1–30 (2025)

2025
[48]

E. D. Coffel, R. M. Horton, A. De Sherbinin, Temperature and humidity based projections of a rapid rise in global heat stress exposure during the 21st century.Environmental Research Letters13(1), 014001 (2017)

2017
[49]

D. J. Vecellio, Q. Kong, W. L. Kenney, M. Huber, Greatly enhanced risk to humans as a consequence of empirically determined lower moist heat stress tolerance.Proceedings of the National Academy of Sciences120(42), e2305427120 (2023)

2023
[50]

Raymond, L

C. Raymond, L. Suarez-Gutierrez, V. Thompson, K. van der Wiel, Distinct favored regions for historical record-setting and future record-breaking humid heat.AGU Advances6(6), e2025A V001963 (2025)

2025
[51]

V. A. Gensini, H. E. Brooks, Spatial trends in United States tornado frequency.npj Climate and Atmospheric Science1(1), 38 (2018)

2018
[52]

Battaglioli, M

F. Battaglioli, M. Taszarek, P. Groenemeijer, T. P´ uˇcik, A. R. R¨adler, Contrasting trends in very large hail events and related economic losses across the globe.Nature Geoscience(2025), doi:https://doi.org/10.1038/s41561-025-01868-0

work page doi:10.1038/s41561-025-01868-0 2025
[53]

Zhang, I

Y. Zhang, I. Held, S. Fueglistaler, Projections of tropical heat stress constrained by atmospheric dynamics.Nature Geoscience14(3), 133–137 (2021)

2021
[54]

M. S. Singh, Z. Kuang, E. D. Maloney, W. M. Hannah, B. O. Wolding, Increasing potential for intense tropical and subtropical thunderstorms under global warming.Proceedings of the National Academy of Sciences114(44), 11657–11662 (2017), doi:https://doi.org/10.1073/ pnas.1707603114

2017
[55]

N. A. Da Silva, J. O. Haerter, Super-Clausius–Clapeyron scaling of extreme precipitation explained by shift from stratiform to convective rain type.Nature Geoscience(2025). 27

2025
[56]

Z. Wang, E. J. Moyer, Robust relationship between midlatitudes CAPE and moist static energy surplus in present and future simulations.Geophysical Research Letters50(14), e2023GL104163 (2023)

2023
[57]

G. J. Zhang, Convective quasi-equilibrium in midlatitude continental environment and its effect on convective parameterization.Journal of Geophysical Research: Atmospheres 107(D14), ACL–12 (2002)

2002
[58]

A. T. LaFleur, R. L. Tanamachi, D. T. Dawson, D. D. Turner, Factors affecting the rapid recovery of CAPE on 31 March 2016 during VORTEX-Southeast.Monthly Weather Review 151(6), 1459–1477 (2023)

2016
[59]

Sillmann,et al., Understanding, modeling and predicting weather and climate extremes: Challenges and opportunities.Weather and climate extremes18, 65–74 (2017)

J. Sillmann,et al., Understanding, modeling and predicting weather and climate extremes: Challenges and opportunities.Weather and climate extremes18, 65–74 (2017)

2017
[60]

T. A. Shaw, B. Stevens, The other climate crisis.Nature639(8056), 877–887 (2025)

2025
[61]

F. Li, T. Tamarin-Brodsky, Atmospheric stability sets maximum moist heat and convection in the midlatitudes.Science Advances12(1), eaea8453 (2026)

2026
[62]

J. R. Buzan, M. Huber, Moist heat stress on a hotter Earth.Annual Review of Earth and Planetary Sciences48(1), 623–655 (2020)

2020
[63]

Zhang, W

Y. Zhang, W. R. Boos, An upper bound for extreme temperatures over midlatitude land. Proceedings of the National Academy of Sciences120(12), e2215278120 (2023)

2023
[64]

S. Q. Duan, F. Ahmed, J. D. Neelin, Moist heatwaves intensified by entrainment of dry air that limits deep convection.Nature Geoscience17(9), 837–844 (2024)

2024
[65]

K. A. Emanuel, J. David Neelin, C. S. Bretherton, On large-scale circulations in convecting atmospheres.Quarterly Journal of the Royal Meteorological Society120(519), 1111–1143 (1994)

1994
[66]

J. D. Neelin, N. Zeng, A quasi-equilibrium tropical circulation model—Formulation.Journal of the atmospheric sciences57(11), 1741–1766 (2000). 28

2000
[67]

M. S. Singh, P. A. O’Gorman, Influence of entrainment on the thermal stratification in simulations of radiative-convective equilibrium.Geophysical Research Letters40(16), 4398– 4403 (2013)

2013
[68]

C. A. Doswell, Severe convective storms—An overview, inSevere convective storms (Springer), pp. 1–26 (2001)

2001
[69]

Tuckman, V

P. Tuckman, V. Agard, K. Emanuel, Evolution of convective energy and inhibition before instances of large CAPE.Monthly Weather Review151(1), 321–338 (2023)

2023
[70]

Tuckman, K

P. Tuckman, K. Emanuel, Origins of Extreme CAPE around the World.Journal of Geophysical Research: Atmospheres129(22), e2024JD041833 (2024)

2024
[71]

R. Wood, C. S. Bretherton, On the relationship between stratiform low cloud cover and lower-tropospheric stability.Journal of climate19(24), 6425–6432 (2006)

2006
[72]

S. A. Klein, A. Hall, J. R. Norris, R. Pincus, Low-cloud feedbacks from cloud-controlling factors: A review.Shallow clouds, water vapor, circulation, and climate sensitivitypp. 135– 157 (2018)

2018
[73]

V. Eyring,et al., Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization.Geoscientific Model Development9(5), 1937–1958 (2016), doi:10.5194/gmd-9-1937-2016,https://gmd.copernicus.org/articles/9/ 1937/2016/

work page doi:10.5194/gmd-9-1937-2016 1937
[74]

T. N. Carlson, S. G. Benjamin, G. S. Forbes, Y. F. Li, Elevated mixed layers in the re- gional severe storm environment: Conceptual model and case studies.Monthly Weather Review111(7), 1453–1474 (1983), doi:https://doi.org/10.1175/1520-0493(1983)111⟨1453: EMLITR⟩2.0.CO;2

work page doi:10.1175/1520-0493(1983)111 1983
[75]

F. Li, D. R. Chavas, K. A. Reed, N. Rosenbloom, D. T. Dawson II, The role of elevated terrain and the Gulf of Mexico in the production of severe local storm environments over North America.Journal of Climate34(19), 7799–7819 (2021). 29

2021
[76]

Raymond,et al., On the controlling factors for globally extreme humid heat.Geophysical Research Letters48(23), e2021GL096082 (2021)

C. Raymond,et al., On the controlling factors for globally extreme humid heat.Geophysical Research Letters48(23), e2021GL096082 (2021)

2021
[77]

J. Chen, A. Dai, Y. Zhang, K. L. Rasmussen, Changes in convective available potential energy and convective inhibition under global warming.Journal of Climate33(6), 2025–2050 (2020)

2025
[78]

Taszarek, J

M. Taszarek, J. T. Allen, M. Marchio, H. E. Brooks, Global climatology and trends in convective environments from ERA5 and rawinsonde data.NPJ climate and atmospheric science4, 1–11 (2021)

2021
[79]

W. S. Ashley, A. M. Haberlie, V. A. Gensini, The future of supercells in the United States. Bulletin of the American Meteorological Society104(1), E1–E21 (2023)

2023
[80]

S. A. Hill,et al., More extreme Indian monsoon rainfall in El Ni ˜no summers.Science 389(6766), 1220–1224 (2025)

2025

Showing first 80 references.