Results 251 to 260 of about 288,014 (296)
Automatic computational classification of bone marrow cells for B cell pediatric leukemia using UMAP. [PDF]
Niño-López A +6 more
europepmc +1 more source
El fenómeno El Niño – Oscilación del Sur (ENOS) - Junio 2018
Laura Soledad Aldeco +2 more
openalex +1 more source
Meta‐analysis of 417 trials shows that El Niño amplifies soybean rust impacts in Brazil. Damage coefficients were higher during El Niño, causing greater yield losses at similar severity, whereas yield protection from management was also greatest, emphasising the value of El Niño‐informed disease outlooks.
Kaique S. Alves +2 more
wiley +1 more source
Predictive modeling of Super El Niño through integrated local and global climate signals. [PDF]
Yoon CH, Park J, Cheoun MK.
europepmc +1 more source
Short Abstract When a positive decision is granted on an asylum claim, a new refugee has limited time before their existing government support (housing, finance) terminates. This transition between legal is variously termed the ‘move‐on period’ or the ‘28‐day gap’.
Sarah M. Hughes
wiley +1 more source
Global climate mode resonance due to rapidly intensifying El Niño-Southern Oscillation. [PDF]
Stuecker MF +8 more
europepmc +1 more source
Abstract Global storm resolving models (GSRMs) represent the next generation of global climate models. One of them is a 5‐km Icosahedral Nonhydrostatic Weather and Climate Model (ICON). Its high resolution means that parameterizations of convection and clouds, including subgrid‐scale clouds, are omitted, relying on explicit simulation but necessarily ...
Peter Kuma +11 more
wiley +1 more source
13-4E62 Improvement in care time for P-HOPf after implementation of golden hour
Diana Toledo Hernández +2 more
doaj +1 more source
ENSO modulates aerobic habitat across varying hypoxia tolerance levels in the Southeast Pacific throughout the twenty-first century. [PDF]
Parouffe A +3 more
europepmc +1 more source
Abstract Future changes in El Niño‐Southern Oscillation (ENSO), the dominant mode of global climate variability, remain uncertain. Accordingly, large ensembles—which allow internally‐generated variations to be averaged out—are essential for assessing the response of ENSO to external forcing.
Arthur Coquereau +3 more
wiley +1 more source

