Zobrazeno 1 - 10
of 357
pro vyhledávání: '"N. Maher"'
Autor:
A. D. King, T. Ziehn, M. Chamberlain, A. R. Borowiak, J. R. Brown, L. Cassidy, A. J. Dittus, M. Grose, N. Maher, S. Paik, S. E. Perkins-Kirkpatrick, A. Sengupta
Publikováno v:
Earth System Dynamics, Vol 15, Pp 1353-1383 (2024)
Under the Paris Agreement, signatory nations aim to keep global warming well below 2 °C above pre-industrial levels and preferably below 1.5 °C. This implicitly requires achieving net-zero or net-negative greenhouse gas emissions to ensure long-ter
Externí odkaz:
https://doaj.org/article/132ca457d5e442688e23b26a74046ca4
Publikováno v:
Ocean Science, Vol 19, Pp 499-515 (2023)
Regional emulation tools based on statistical relationships, such as pattern scaling, provide a computationally inexpensive way of projecting ocean dynamic sea-level change for a broad range of climate change scenarios. Such approaches usually requir
Externí odkaz:
https://doaj.org/article/1a96d3b3b77d4a3ba0bfaaf0bf6e77a2
Autor:
N. Maher, R. C. J. Wills, P. DiNezio, J. Klavans, S. Milinski, S. C. Sanchez, S. Stevenson, M. F. Stuecker, X. Wu
Publikováno v:
Earth System Dynamics, Vol 14, Pp 413-431 (2023)
Future changes in the El Niño–Southern Oscillation (ENSO) are uncertain, both because future projections differ between climate models and because the large internal variability of ENSO clouds the diagnosis of forced changes in observations and in
Externí odkaz:
https://doaj.org/article/b0c42a0500234266b460140c4c27967a
Publikováno v:
Earth System Dynamics, Vol 13, Pp 1289-1304 (2022)
The El Niño–Southern Oscillation (ENSO) occurs in three phases: neutral, warm (El Niño), and cool (La Niña). While classifying El Niño and La Niña is relatively straightforward, El Niño events can be broadly classified into two types: central
Externí odkaz:
https://doaj.org/article/6ea0947b177d40219794ece02d4cafb5
Publikováno v:
Earth System Dynamics, Vol 12, Pp 975-996 (2021)
Using the Max Planck Institute Grand Ensemble (MPI-GE) with 200 members for the historical simulation (1850–2005), we investigate the impact of the spatial distribution of volcanic aerosols on the El Niño–Southern Oscillation (ENSO) response. In
Externí odkaz:
https://doaj.org/article/510414a9599042c596b2c04ff4b55023
Publikováno v:
Earth System Dynamics, Vol 12, Pp 401-418 (2021)
Single model initial-condition large ensembles (SMILEs) are valuable tools that can be used to investigate the climate system. SMILEs allow scientists to quantify and separate the internal variability of the climate system and its response to externa
Externí odkaz:
https://doaj.org/article/b556066a3fc342e8a45da628af229856
Publikováno v:
Earth System Dynamics, Vol 11, Pp 885-901 (2020)
Initial-condition large ensembles with ensemble sizes ranging from 30 to 100 members have become a commonly used tool for quantifying the forced response and internal variability in various components of the climate system. However, there is no conse
Externí odkaz:
https://doaj.org/article/f5b5956df75a4839b88f617ecfbf23cd
Publikováno v:
Earth System Dynamics, Vol 11, Pp 491-508 (2020)
Partitioning uncertainty in projections of future climate change into contributions from internal variability, model response uncertainty and emissions scenarios has historically relied on making assumptions about forced changes in the mean and varia
Externí odkaz:
https://doaj.org/article/fc7b77fd30d64bccaa62197a49c82a46
Autor:
Hyun-ju Lee, Jin-Hee Park, Justin H. Trotter, James N. Maher, Kathleen E. Keenoy, You Mi Jang, Youngeun Lee, Jae-Ick Kim, Edwin J. Weeber, Hyang-Sook Hoe
Publikováno v:
Experimental Neurobiology. 32:42-55
Publikováno v:
International journal of electrical and computer engineering systems
Volume 14
Issue 1
Volume 14
Issue 1
The Brain Computer Interface (BCI) has a great impact on mankind. Many researchers have been trying to employ different classifiers to figure out the human brain's thoughts accurately. In order to overcome the poor performance of a single classifier,