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6 results for “El Niño-Southern Oscillation”

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zenodo36/100

Data for "Strong linkage of El Niño-Southern Oscillation to the polar cold air mass in the Northern Hemisphere"

<p>This repository archives codes for analysis and plot presented in Abdillah et al. (2018):&nbsp;&quot;Strong linkage of El Ni&ntilde;o-Southern Oscillation to the polar cold air mass in the Northern Hemisphere&quot;. The codes are written in GrADS, Octave, and NCL format.&nbsp;</p> <p>The repository also includes&nbsp;a Fortran package for isentropic polar cold air mass diagnosis as in Iwasaki et al. (2014). The package was specifically created by Dr. Y. Kanno.</p> <p>Reference:</p> <p>Abdillah, M. R., Kanno, Y., Iwasaki, T. (2018).&nbsp;Strong linkage of El Ni&ntilde;o‐Southern Oscillation to the polar cold air mass in the Northern Hemisphere. <em>Geophysical Research Letters, in press.&nbsp;</em>https://doi.org/10.1029/2018GL077612</p> <p>Iwasaki, T., Shoji, T., Kanno, Y., Sawada, M., Ujiie, M., &amp; Takaya, K. (2014). Isentropic Analysis of Polar Cold Airmass Streams in the Northern Hemispheric Winter. <em>Journal of the Atmospheric Sciences</em>, <em>71</em>(6), 2230&ndash;2243. https://doi.org/10.1175/JAS-D-13-058.1</p>

opencc-by-4.0May 2018View details →
dryad32/100

Data from: Breaking out of the comfort zone: El Niño-Southern Oscillation as a driver of trophic flows in a benthic consumer of the Humboldt Current ecosystem

The trophic flow of a species is considered a characteristic trait reflecting its trophic position and function in the ecosystem and its interaction with the environment. However, climate patterns are changing and we ignore how patterns of trophic flow are being affected. In the Humboldt Current ecosystem, arguably one of the most productive marine systems, El Niño-Southern Oscillation is the main source of interannual and longer-term variability. To assess the effect of this variability on trophic flow we built a 16-year series of mass-specific somatic production rate (P/B) of the Peruvian scallop (Argopecten purpuratus), a species belonging to a former tropical fauna that thrived in this cold ecosystem. A strong increase of the P/B ratio of this species was observed during nutrient-poor, warmer water conditions typical of El Niño, owing to the massive recruitment of fast-growing juvenile scallops. Trophic ecology theory predicts that when primary production is nutrient limited, the trophic flow of organisms occupying low trophic levels should be constrained (bottom-up control). For former tropical fauna thriving in cold, productive upwelling coastal zones, a short time of low food conditions but warm waters during El Niño could be sufficient to waken their ancestral biological features and display massive proliferations.

opencc-zeroDec 2016View details →
zenodo32/100

Changes in BVOC emissions in response to the El Niño-Southern Oscillation | Data & scripts

<p>Data and Python scripts used for the study &quot;Changes in BVOC emissions in response to the El Ni&ntilde;o-Southern Oscillation&quot; Vella et al. Preprint published on EGUSphere on 03 May 2023.</p>

opencc-by-4.0May 2023View details →
zenodo32/100

The Potential Influence of Maritime Continent Deforestation on El Niño-Southern Oscillation: Insights from Idealized Modeling Experiments

<p>Codes for the Figures and Tables shown in the paper &quot;The Potential Influence of Maritime Continent Deforestation on El Ni&ntilde;o-Southern Oscillation: Insights from Idealized Modeling Experiments&quot;</p> <p>Also, the restart and initial data are used to drive CESM1.</p>

opencc-by-4.0Jun 2023View details →
dryad32/100

Data from: Breaking out of the comfort zone: El Niño-Southern Oscillation as a driver of trophic flows in a benthic consumer of the Humboldt Current ecosystem

Open the record for dataset details and reuse information.

publicMay 2017View details →
zenodo28/100

Data and analysis code for "Increased frequency of multi-year El Niño-Southern Oscillation events across the Holocene"

<p>Data and analysis code for "Increased frequency of multi-year El Ni&ntilde;o-Southern Oscillation events across the Holocene"&nbsp;</p> <p>In "Zenodo.zip",</p> <ul> <li>Code to produce the main figures (Figs. 1-4) in the manuscript: Matlab code named as Fig#_202411.m</li> <li>Other Matlab functions used in the code&nbsp;</li> <li>Nino 3.4 monthly surface (sea/air) temperature data: 8 NetCDF files named Model-Name_variable_N34_mon_final.nc for 8 transient Holocene simulations</li> <li>Tropical Pacific climatological surface temperature and ocean subsurface temperature: processed as Tpac_tmp_response or Tsub_Model-name_response in MAT(matlab) format&nbsp;</li> <li>Nino 3.4 and 1+2 SST anomalies from ERSST.v5: N1234_ersst_1854_2023 in MAT format</li> <li>Central Pacific fossil coral data from Grothe et al. 2020 (accessed at https://www.ncei.noaa.gov/access/paleo-search/study/22415)</li> <li>Other MAT files temporarily generated for figure plots</li> </ul>

opencc-by-4.0Oct 2024View details →

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