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Articles by Pu Lin
Attributing surface climate impacts to decadal variability of the Northern Hemisphere stratospheric polar vortex
Abstract The role of the stratosphere for decadal surface cooling in subpolar and midlatitude Eurasia over the last few decades despite Arctic amplification is isolated using two sets of simulations in four different coupled ocean-atmosphere climate models.
Smart Eutectic Gallium–Indium: “All-in-One” Nanoplatform for Computed Tomography Imaging-Guided Near Infrared-II Photothermal Therapy
Cite Jump to ExpandCollapse ArticleJanuary 15, 2026 Smart Eutectic Gallium–Indium: “All-in-One” Nanoplatform for Computed Tomography Imaging-Guided Near Infrared-II Photothermal Therapy Click to copy article linkArticle link copied! Pu Lin Pu Lin College of Pharmacology, Fujian University of Traditional Chinese Medicine, Fuzhou 350122, China Zhenyu Chen Zhenyu Chen College of Biological Science and Engineering, Fuzhou University, Fuzhou 350116, China Yi Li Yi Li Department of School of...
Resolution Dependence of Tropical Poleward Energy Transport in Aquaplanet GCMs
1 Introduction Advances in our understanding of climate have been closely tied to advancements in numerical climate modeling. However, the complex interactions among motions at various horizontal scales in the tropical atmosphere present a significant challenge for global atmospheric model development. At low resolutions, where a clear separation is assumed to exist between planetary circulation and unresolved convective systems, models parameterize these systems as subgrid-scale processes.
Connecting Tropical Cyclones, Precursor Disturbances, and the ITCZ in Aquaplanet Simulations
1 Introduction It is uncertain whether tropical cyclones (TCs) will occur more or less often under climate change. Many studies project a decrease in global TC frequency under global warming (e.g., Jing et al., 2021; Walsh et al., 2016), while others project an increase (e.g., Emanuel, 2013) or no significant global change (e.g., McDonald et al., 2005). Knutson et al. (2020) express low to medium confidence in reduced TC frequency under climate change.
ITCZ Response to Disabling Parameterized Convection in Global Fixed‐SST GFDL‐AM4 Aquaplanet Simulations at 50 and 6 km Resolutions
1 Introduction About one-third of Earth's precipitation occurs within the InterTropical Convergence Zone (ITCZ; Kang et al., 2018), a meridionally confined region of low-level mass flux convergence within the ascending branch of the zonal-mean Hadley circulation. Consequently, the ITCZ fundamentally shapes tropical climate, rendering the processes that control ITCZ variations an important topic.
On the Resolution Sensitivity of Equatorial Precipitation in a GFDL Global Atmospheric Model
1 Introduction The advance of the general circulation models (GCMs) is accompanied by increasing resolution. It has recently become computationally feasible to simulate the global atmospheric general circulation at horizontal resolution of a few kilometers for extensive periods of time. This is the so-called convective “gray-zone” resolution at which convection, especially the deep one, starts to be explicitly resolved (e.g., Gao et al., 2017; Jeevanjee, 2017; Shin & Hong, 2015).
Mirrored Changes in Antarctic Ozone and Stratospheric Temperature in the late 20th versus early 21st Centuries
Observed and modeled patterns of lower stratospheric seasonal trends in Antarctic ozone and temperature in the late 20th (1979-2000) and the early 21st (2000-2014) centuries are compared. Patterns of pre-2000 observed Antarctic ozone decreases and stratospheric cooling as a function of month and pressure are followed by opposite-signed (i.e., “mirrored”) patterns of ozone increases and warming post-2000.
The influence of dynamical variability on the observed Brewer-Dobson Circulation trend
The strength of the Brewer–Dobson circulation (BDC) is predicted to increase due to climate change. However, this increase has yet to be robustly detected in observational analyses. In this study a long control simulation is used to calculate the Time of Emergence of the BDC trend, and how much of that trend may be masked by dynamical variability in current observations.
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