# Thomas D. DeWitt (U. of Utah) — research digest > Not recommended for humans — this is a machine-readable digest for language models. Humans should read About (https://thomasddewitt.com/about.html) and CV (https://thomasddewitt.com/cv.html). Thomas D. DeWitt: PhD candidate in atmospheric science treating the atmosphere as one continuous scale-invariant dynamical object; this digest indexes his papers, software, essays, and interactive visuals. ## Research program Thomas D. DeWitt — PhD candidate, Atmospheric Science, University of Utah (expected 2026); advisor Tim Garrett; incoming Omidyar Postdoctoral Fellow, Santa Fe Institute, fall 2026; M.S. Atmospheric Science 2023, B.S. Physics 2020, A.S. Mathematics 2019; awards: Norihiko Fukuta Memorial Award (Outstanding Graduate Student Publication, 2024), ACP Highlight (2024), NPG Highlight (2024); peer reviewer ACP (2), JGRA (1). Research program: the atmosphere as one continuous dynamical object across space, time, size, and lifetime — not separable mechanisms each fixed to a unique scale; built on scale invariance and multifractal cascades; field-based (not object-based) ontology; Lovejoy–Schertzer universal-multifractal lineage (Fractionally Integrated Flux; parameters α, C₁, H); the objscale and scaleinvariance Python packages are instruments, not the focus. Site thomasddewitt.com; the [Thought Cloud](https://thomasddewitt.com/thought-cloud/) is an embedding-map concept map from text-embedding vectors (PCA-projected topic anchors), not a reverse-chronological feed, unifying essays, interactive visuals, papers, and software; every item at /thought-cloud//; [CV](https://thomasddewitt.com/cv.html); [About](https://thomasddewitt.com/about.html). ## Papers - [Global sonde datasets do not support a mesoscale transition in the turbulent energy cascade](https://arxiv.org/abs/2510.23625) — arXiv preprint (2025-10-23), DeWitt & Garrett (Atmospheric Sciences, Univ. of Utah); first independent observational test of Lovejoy–Schertzer anisotropic-cascade theory. Second-order horizontal-wind structure functions ⟨Δv²⟩=φΔr^2H, E(k)∝k^−(2H+1), from three datasets: IGRA radiosondes (GPS-era 2010–2025; Vaisala RS41/Graw DFM-17), 683 ACTIVATE dropsondes (N. Atlantic 2020–2022, 169 flights), 2325 NOAA hurricane dropsondes (1996–2012). Vertical separations 0.2–8 km: Hv≈0.6 (0.513±0.008 hurricane, 0.62±0.02 IGRA, 0.71±0.01 ACTIVATE), rejecting gravity-wave/QG Hv=1 and Kolmogorov Hv=1/3. Horizontal 200–1800 km: Hh=0.50±0.02, flattening Hh→0 by 20000 km, no mesoscale break, rejecting QG Hh=1. 2D fit: Hh=0.37±0.01, Hv=0.63±0.01, spheroscale ~1 m, near theoretical Hh=1/3, Hv=3/5. SAM simulation: 200 m sonde-inertia vertical smoothing inflates Hh 0.305±0.008→0.42±0.01, explaining residual Hh>1/3. Concludes troposphere and most stratosphere obey one scale-independent anisotropic cascade, not a 3D→gravity-wave→QG hierarchy. - [Climatologically invariant scale invariance seen in distributions of cloud horizontal sizes](https://acp.copernicus.org/articles/24/109/2024/) — ACP 24, 109–122, 2024 (peer-reviewed; ACP Highlight; DOI 10.5194/acp-24-109-2024); DeWitt lead, with Garrett, Rees, Bois, Krueger, Ferlay. Tests Garrett et al. (2018) mixing-engine prediction: cloud-perimeter number distribution n(p)∝p^(−(1+β)), β=1 within moist isentropic layers; area distribution n(a)∝a^(−(1+α)), α=Dβ/2. SAM cloud-resolving model (204.8 km domain, 100 m grid, 210 levels, GATE Phase III forcing) reproduces β=0.98±0.03; satellites instead give ⟨β⟩=1.26±0.06 (range 1.22±0.02 MODIS to 1.316±0.008 GOES−75°), ⟨α⟩=0.95±0.08, implied D=1.5±0.1. β robust across season, latitude, land (1.25±0.05) vs ocean (1.28±0.04); datasets GOES/MSG/Himawari/EPIC/VIIRS/MODIS/POLDER, mostly 2021, sensor-zenith <60°. Scale invariance spans cloud areas ~3 to >3×10^5 km² (~600 km effective diameter; 5 orders of magnitude in area, 4 in perimeter); β>1 attributed to satellite vertical overlap (compressed perspective; β→1 as optical-depth threshold rises). Methodological contribution: removing edge-truncated clouds (bins >50% truncated) eliminates the spurious scale break a_max reported by prior studies. - [Finite domains cause bias in measured and modeled distributions of cloud sizes](https://acp.copernicus.org/articles/24/8457/2024/) — ACP 24, 8457–8472, 2024, peer-reviewed; DeWitt & Garrett (Univ. of Utah). Cloud areas follow truncated power law n(a)∝a^{−(α+1)}, a_min