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179 results for “niños”

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zenodo44/100

mom6 cobalt model result for oceanic carbon response to El Niños

GEOS_Chem atmospheric transport model, monthly, 2.5 degree resolution in tropical Pacific Ocean (120-300E, 30N-30S) 1. GEOS_Chem_tropical_pacific_monthly_clim_1992_2017.nc 2. GEOS_Chem_tropical_pacific_monthly_iav_1992_2017.nc 1 and 2 are GEOS_Chem atmospheric transport model results MOM6 COBALT model results Note1: region range is 120-300E, 30N-30S with a resolution of half degree, monthly result from 1982.1.1 to 2018.1.1 Note2: if the file name has a label "_detrend_deseason", this file is detrended and deseasonized using full value in 1982-2018 with CDO "cdo -ymonsub -detrend $fin -ymonmean -detrend $fin $fout" Note3: ocean/sea surface is the first layer which is 1 meter deep Note4: MLD_001_temp/salt/dic/alk/kd is the vertical mean value in the mixing layer depth (criterial of 0.01 kg/m3) MOM6_COBALT_tropical_pacific_monthly_dic_deltap_1982_2018_detrend_deseason.nc     (detrended and deseasonalized delta pCO2 (ocean pCO2 minus air pCO2) in the ocean surface) MOM6_COBALT_tropical_pacific_monthly_dic_deltap_1982_2018.nc     (delta pCO2 (ocean pCO2 minus air pCO2) in the ocean surface) MOM6_COBALT_tropical_pacific_monthly_dic_stf_1982_2018_detrend_deseason.nc     (detrended and deseasonalized air-sea CO2 flux, positive to ocean) MOM6_COBALT_tropical_pacific_monthly_dic_stf_1982_2018.nc     (air-sea CO2 flux, positive to ocean) MOM6_COBALT_tropical_pacific_monthly_MLD_001_1982_2018.nc     (Mixing layer depth with a density criterial of 0.01 kg/m3) MOM6_COBALT_tropical_pacific_monthly_MLD_001_alk_1982_2018_detrend_deseason.nc     (first compute vertical mean alkilinity in the mixing layer depth (criterial of 0.01 kg/m3), then do detrended and deseasonalized) MOM6_COBALT_tropical_pacific_monthly_MLD_001_alk_zgradient_1982_2018_detrend_deseason.nc     (first compute vertical mean alkilinity gradient (dalk/dz) in the mixing layer depth (criterial of 0.01 kg/m3), then do detrended and deseasonalized) MOM6_COBALT_tropical_pacific_monthly_MLD_001_dic_1982_2018_detrend_deseason.nc     (first compute vertical mean dissolved inorganic carbon (DIC) in the mixing layer depth (criterial of 0.01 kg/m3), then do detrended and deseasonalized) MOM6_COBALT_tropical_pacific_monthly_MLD_001_dic_zgradient_1982_2018_detrend_deseason.nc     (first compute vertical mean DIC (ddic/dz) in the mixing layer depth (criterial of 0.01 kg/m3), then do detrended and deseasonalized) MOM6_COBALT_tropical_pacific_monthly_MLD_001_Kd_interface_1982_2018_detrend_deseason.nc     (first compute vertical mean Diapycnal diffusivity at interfaces layers (kd_interface) in the mixing layer depth (criterial of 0.01 kg/m3), then do detrended and deseasonalized) MOM6_COBALT_tropical_pacific_monthly_MLD_001_salt_1982_2018_detrend_deseason.nc     (first compute vertical mean salinity in the mixing layer depth (criterial of 0.01 kg/m3), then do detrended and deseasonalized) MOM6_COBALT_tropical_pacific_monthly_MLD_001_temp_1982_2018_detrend_deseason.nc     (first compute vertical mean temperature in the mixing layer depth (criterial of 0.01 kg/m3), then do detrended and deseasonalized) MOM6_COBALT_tropical_pacific_monthly_MLD_001_u_1982_2018_detrend_deseason.nc     (first compute vertical mean velocity u in the mixing layer depth (criterial of 0.01 kg/m3), then do detrended and deseasonalized) MOM6_COBALT_tropical_pacific_monthly_MLD_001_v_1982_2018_detrend_deseason.nc     (first compute vertical mean velocity v in the mixing layer depth (criterial of 0.01 kg/m3), then do detrended and deseasonalized) MOM6_COBALT_tropical_pacific_monthly_MLD_003_1982_2018.nc     (Mixing layer depth with a density criterial of 0.03 kg/m3) MOM6_COBALT_tropical_pacific_monthly_pco2surf_1982_2018_detrend_deseason.nc     (detrended and deseasonalized sea surface pCO2 (ocean pCO2)) MOM6_COBALT_tropical_pacific_monthly_pco2surf_1982_2018.nc     (sea surface pCO2 (ocean pCO2)) MOM6_COBALT_tropical_pacific_monthly_sfc_chl_1982_2018.nc     (sea surface chlorophyll) MOM6_COBALT_tropical_pacific_monthly_sfc_dic_1982_2018.nc     (sea surface dissolved inorganic carbon (DIC)) MOM6_COBALT_tropical_pacific_monthly_sfc_no3_1982_2018.nc     (sea surface nitrate, NO3) MOM6_COBALT_tropical_pacific_monthly_sfc_po4_1982_2018.nc     (sea surface phosphate, PO4) MOM6_COBALT_tropical_pacific_monthly_SSS_1982_2018.nc     (sea surface salinity) MOM6_COBALT_tropical_pacific_monthly_SST_1982_2018.nc     (sea surface temperature) MOM6_COBALT_tropical_pacific_monthly_taux_1982_2018_detrend_deseason.nc     (detrended and deseasonalized wind stress in zonal direction) MOM6_COBALT_tropical_pacific_monthly_taux_1982_2018.nc     (wind stress in zonal direction) MOM6_COBALT_tropical_pacific_monthly_tauy_1982_2018_detrend_deseason.nc     (detrended and deseasonalized wind stress in meridional direction) MOM6_COBALT_tropical_pacific_monthly_tauy_1982_2018.nc     (wind stress in meridional direction) MOM6_COBALT_tropical_pacific_monthly_tc_depth_1982_2018.nc     (thermocline depth defined as depth where the temperature equals 20oC) JRA_rain_tropical_pacific_monthly_prrn_1982_2018_detrend_deseason.nc (detrended and deseasonalized JRA rainfall)   Budget terms based MOM6 COBALT model results Note1: region range is 120-300E, 30N-30S with a resolution of half degree, monthly result from 1982.1.1 to 2018.1.1 Note2: this is the vertical mean result in the mixing layer depth (criterial of 0.01 kg/m3) after detrend and deseasonalize MOM6_COBALT_tropical_pacific_monthly_MLD_001_pco2w_budget_1982_2018_detrend_deseason.nc     (budget terms used for ocean pCO2 budget analysis, vertical mean in the mixing layer depth (criterial of 0.01 kg/m3), then do detrended and deseasonalized) pco2_hadv_hdif: horizontal transport term, H_circ; dpco2_hadvx: zonal advection term; dpco2_hadvy: meridional advection term; dpco2_hdif: horizontal diffusivity term; dpco2_vadv_vdif: vertical transport term; dpco2_dic_vdif_vdif: vertical transport term induced by DIC; dpco2_alk_vdif: vertical transport term induced by Alk; dpco2_bio: biological term dpco2_rain: surface freshwater term dpco2_sst: thermal term dpco2_dt: pco2 response term dpco2_flux: CO2 flux response term

opencc-by-4.0Feb 2020View details →

zenodo44/100

El Niño Enhances Snowline Rise and Ice Loss on the Quelccaya Ice Cap, Peru

El Niño Enhances Snowline Rise on the Quelccaya Ice Cap, Peru (in-review) Kara A. Lamantia, Laura J. Larocca, Lonnie G. Thompson, Bryan Mark Exported results from automated snow cover area detection on the Quelccaya Ice Cap (QIC). Further calculated results are detailed in the supplementary documentation in the draft manuscript. See READ ME.txt file for details Sample Code available for Landsat 8 imagery here at the following URL: https://code. earthengine.google.com/cfcbd0780ff3f09b0698035cd6dd678a

opencc-by-4.0Mar 2024View details →

zenodo44/100

Data and code: Disentangling the impact of Atlantic Niño on sea-air CO2 flux

This repository share (1) post-processed data of Norwegian Earth system model version 2 (LM) and (2)  codes for calculating carbon system from NorESM variables (MATLAB format).

opencc-by-4.0Mar 2023View details →

edi44/100

MCR LTER: Coral Reef: Recruitment during El Niño, Edmunds PLOS1 2017

The negative implications of the thermal sensitivity of reef corals became clear with coral bleaching throughout the Caribbean in the 1980’s, and later globally, with the severe El Niño of 1998 and extensive seawater warming in 2005. These events have substantially contributed to declines in coral cover, and therefore the El Niño of 2016 raised concerns over the implications for coral reefs; on the Great Barrier Reef these concerns have been realized. A different outcome developed in Mo’orea, French Polynesia, where in situ seawater temperature from 15 March 2016 to 15 April 2016 was an average of 0.4°C above the upper 95% CI of the decadal mean temperature, and the NOAA Degree Heating Weeks (DHW) metric supported a Level 1 bleaching alert (DHW ≥ 4.0). Starting 1 September 2016 and for the rest of the year (122 d), in situ seawater temperature was an average of 0.4°C above the 95% CI of long-term values, although DHW remained at zero. Minor coral bleaching (0.2–2.6% of the coral) occurred on the outer reef (10-m and 17-m depth) in April 2016, by May 2016 it had intensified to affect 1.3– 16.8% of the coral, but by August 2016, only 1.4–3.0% of the coral was bleached. Relative to the previous decade, recruitment of scleractinians to settlement tiles on the outer- (10 m) and back- (2 m) reef over 2016/17 was high, both from January 2016 to August 2016, and from August 2016 to January 2017, with increased relative abundances of pocilloporids on the outer reef, and acroporids in the back reef. The 2016 El Niño created a distinctive signature in seawater temperature for Mo’orea, but it did not cause widespread coral bleaching or mortality, rather, it was associated with high coral recruitment. While the 2016 El Niño has negatively affected other coral reefs in the Indo-Pacific, the coral communities of Mo’orea continue to show signs of resilience, thus cautioning against general statements regarding the effects of the 2015/16 El Niño on coral reefs in the region. This wo

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Dataset results

mom6 cobalt model result for oceanic carbon response to El Niños

El Niño Enhances Snowline Rise and Ice Loss on the Quelccaya Ice Cap, Peru

Data and code: Disentangling the impact of Atlantic Niño on sea-air CO2 flux

MCR LTER: Coral Reef: Recruitment during El Niño, Edmunds PLOS1 2017

FIGURE 4 in Heterobranch Sea Slug Range Shifts in the Northeast Pacific Ocean associated with the 2015-16 El Niño

Effects of the 2015-2016 El Niño on Currents and Temperatures on the Northern Peruvian Coast

MOM6-COBALT2 model results for asymmetrical Ocean Carbon Responses to La Niña and El Niño in the Tropical Pacific Ocean

Daily Anomalies and High Productivity Zone Mask for Northern Peruvian Coastal Marine Ecosystem during the 2017 Coastal El Niño (December 2016 - May 2017)

Dataset for manuscript "El Niño Southern Oscillation and Tropical Basin Interaction in Idealized Worlds"

Fig. 6 in Population dynamics of the migratory fish Prochilodus lineatus in a neotropical river: the relationships with river discharge, flood pulse, El Niño and fluvial megafan behaviour

Fig. 5 in Population dynamics of the migratory fish Prochilodus lineatus in a neotropical river: the relationships with river discharge, flood pulse, El Niño and fluvial megafan behaviour

Fig. 4 in Population dynamics of the migratory fish Prochilodus lineatus in a neotropical river: the relationships with river discharge, flood pulse, El Niño and fluvial megafan behaviour

Fig. 3 in Population dynamics of the migratory fish Prochilodus lineatus in a neotropical river: the relationships with river discharge, flood pulse, El Niño and fluvial megafan behaviour

Fig. 6 in Spatial and temporal variation of benthic fish assemblages during the extreme drought of 1997-98 (El Niño) in the middle rio Negro, Amazonia, Brazil

Fig. 5. Estimated species richness E in Spatial and temporal variation of benthic fish assemblages during the extreme drought of 1997-98 (El Niño) in the middle rio Negro, Amazonia, Brazil

Fig. 3. Estimated species richness E in Spatial and temporal variation of benthic fish assemblages during the extreme drought of 1997-98 (El Niño) in the middle rio Negro, Amazonia, Brazil

Fig. 4 in Spatial and temporal variation of benthic fish assemblages during the extreme drought of 1997-98 (El Niño) in the middle rio Negro, Amazonia, Brazil

Emotional Quotient Inventory - Young Version / Inventario de Inteligencia Emocional - Versión para Niños // EMOTIONAL INTELLIGENCE-EQi-YV_Data_IC_T6-Post

Emotional Quotient Inventory - Young Version / Inventario de Inteligencia Emocional – Versión para Niños // EMOTIONAL INTELLIGENCE-EQi-YV_Data_IC_T3-Post

Emotional Quotient Inventory - Young Version / Inventario de Inteligencia Emocional – Versión para Niños // EMOTIONAL INTELLIGENCE-EQi-YV_Data_CC-CS_T6-Post

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