NorESM1-Happi slab ocean climate sensitivity experiments
type: Nanopublication
has assertion: assertion
has provenance: provenance
has publication info: pubinfo
type: RoCrateNanopub
created: 2026-03-03T16:16:47.296+01:00
creator: RoCrateBot

Environmental research
type: DefinedTerm

Life sciences
type: DefinedTerm

Physical sciences
type: DefinedTerm

Earth sciences
type: DefinedTerm

service-account-enrichment
type: Agent

NorESM1-Happi slab ocean climate sensitivity experiments
type: ResearchObject
type: LiveRO
type: Dataset
type: DataResearchObject
about: Environmental research
about: Life sciences
about: Physical sciences
about: Earth sciences
content size: 25515
date created: 2022-03-22 01:07:40.543485+00:00
date modified: 2025-03-05 12:48:07.986184+00:00
date published: 2022-03-22 01:07:40.543485+00:00
description: These experiments are used to calculate the climate sensitivity of NorESM1-Happi with a slab ocean configuration. Consists of a 1850 control simulation with slab ocean q-fluxes derived from the NorESM1-Happi fully coupled 1850 control. A 2xCO2 experiment, and a 4xCO2 experiment. Those two experiments use the same q-flux field as the control simualtion, so the only forcing that is changed is the CO2 concentration in the atmosphere. Data description: case = N1Happi_som_1850_02; N1Happi_som_1850_2XCO2_02; N1Happi_som_1850_4XCO2_01; Source = CAM ; Variables = P0:reference pressure ; lat:latitude ; lon:longitude ; slat:staggered latitude ; slon:staggered longitude ; w_stag:staggered latitude weights ; lev:hybrid level at midpoints (1000*(A+B)) ; ilev:hybrid level at interfaces (1000*(A+B)) ; isccp_prs:Mean ISCCP pressure ; isccp_tau:Mean ISCCP optical depth ; isccp_prstau:Mean pressure (mb).mean optical depth (unitless)/1000 ; time:time ; time_bnds:time interval endpoints ; ntrm:spectral truncation parameter M ; ntrn:spectral truncation parameter N ; ntrk:spectral truncation parameter K ; ndbase:base day ; nsbase:seconds of base day ; nbdate:base date (YYYYMMDD) ; nbsec:seconds of base date ; mdt:timestep ; nlon:number of longitudes ; wnummax:cutoff Fourier wavenumber ; hyai:hybrid A coefficient at layer interfaces ; hybi:hybrid B coefficient at layer interfaces ; hyam:hybrid A coefficient at layer midpoints ; hybm:hybrid B coefficient at layer midpoints ; gw:gauss weights ; ndcur:current day (from base day) ; nscur:current seconds of current day ; date:current date (YYYYMMDD) ; co2vmr:co2 volume mixing ratio ; ch4vmr:ch4 volume mixing ratio ; n2ovmr:n2o volume mixing ratio ; f11vmr:f11 volume mixing ratio ; f12vmr:f12 volume mixing ratio ; sol_tsi:total solar irradiance ; datesec:current seconds of current date ; nsteph:current timestep ; ABSVIS:Aerosol absorptive optical depth at 0.35-0.64um ; AEROD_v:Total Aerosol Optical Depth in visible band ; AKCXS:Scheme excess ae…
encoding format: application/ld+json
license: no-permission
creation mode: MANUAL
concept: aerosol
concept: carbon dioxide
concept: carbon
concept: climate sensitivity
concept: concentration
concept: control condition
concept: control
concept: experiment
concept: flux
concept: forcing
concept: humidity
concept: land
concept: rain
concept: simulation
concept: slab
concept: snow
concept: temperature
field of research: earth sciences
IPTC: Climate change
IPTC: Weather statistic
IPTC: Weather
lemma: NorESM1-Happi
lemma: aerosol
lemma: climate sensitivity
lemma: control
lemma: experiment
lemma: flux
lemma: forcing
lemma: heat flux
lemma: humidity
lemma: simulation
lemma: snow
lemma: soil
lemma: temperature
NASA: geosciences
phrase: climate sensitivity experiment
phrase: control simulation
phrase: ice surface temperature
phrase: ocean climate sensitivity experiment
phrase: slab ocean configuration
phrase: slab ocean q-flux
phrase: snow albedo
phrase: snow conversion
phrase: snow melt
phrase: snowfall rate
sentence: Consists of a 1850 control simulation with slab ocean q-fluxes derived from the NorESM1-Happi fully coupled 1850 control.
sentence: Data description: case = N1Happi_som_1850_02; N1Happi_som_1850_2XCO2_02; N1Happi_som_1850_4XCO2_01; Source = CAM; Variables = P0:reference pressure; lat:latitude; lon:longitude; slat:staggered latitude; slon:staggered longitude; w_stag:staggered latitude weights; lev:hybrid level at midpoints (1000* A+B); ilev:hybrid level at interfaces (1000* A+B); isccp_prs:Mean ISCCP pressure; isccp_tau:Mean ISCCP optical depth; isccp_prstau:Mean pressure (mb) mean optical depth (unitless) 1000; time:time; time_bnds:time interval endpoints; ntrm:spectral truncation parameter M; ntrn:spectral truncation parameter N; ntrk:spectral truncation parameter K; ndbase:base day; nsbase:seconds of base day; nbdate:base date (YYYYMMDD); nbsec:seconds of base date; mdt:timestep; nlon:number of longitudes; wnummax:cutoff Fourier wavenumber; hyai:hybrid A coefficient at layer interfaces; hybi:hybrid B coefficient at layer interfaces; hyam:hybrid A coefficient at layer midpoints; hybm:hybrid B coefficient at layer midpoints; gw:gauss weights; ndcur:current day (from base day); nscur:current seconds of current day; date:current date (YYYYMMDD); co2vmr:co2 volume mixing ratio; ch4vmr:ch4 volume mixing ratio; n2ovmr:n2o volume mixing ratio; f11vmr:f11 volume mixing ratio; f12vmr:f12 volume mixing ratio; sol_tsi:total solar irradiance; datesec:current seconds of current date; nsteph:current timestep; ABSVIS:Aerosol absorptive optical depth at 0.35-0.64um; AEROD_v:Total Aerosol Optical Depth in visible band; AKCXS:Scheme excess aerosol mass burden; AODVIS:Aerosol optical depth at 0.35-0.64um; BAK:Aerosol extinction; BC:Concentration; BC_A:BC_A; BC_AC:BC_AC; BC_AI:BC_AI; BC_AX:BC_AX; BC_N:BC_N; BC_NI:BC_NI; CABSVIS:Clear air aerosol absorptive optical depth; CAODVIS:Clear air aerosol optical depth; CDNC:Cloud Droplet Number Concentration; CDNCINT:Cloud Droplet Number Column; CDNCIX:Aerosol calc cloud droplet number concentration; CH2O2:H2O2 MMR from file; CLDFOC:Frequency of Warm Cloud Occurence; CLDF…
sentence: Those two experiments use the same q-flux field as the control simualtion, so the only forcing that is changed is the CO2 concentration in the atmosphere.
time reference: 1850
time reference: a 1850
domain: astronomy
domain: physics
domain: scientific terms
organization: Financial Services Authority
organization: Transportation Security Administration
place: British Columbia
place: Quebec
place: United States of America
place: Washington State
cite-as: Jens Boldingh Debernard. "NorESM1-Happi slab ocean climate sensitivity experiments." ROHub. Mar 22 ,2022. https://w3id.org/ro-id/33bc542c-0486-4ede-8084-e214390cb615.

metadata
type: Folder
type: Dataset

data
type: Folder
type: Dataset

biblio
type: Folder
type: Dataset

raw data
type: Folder
type: Dataset

https://w3id.org/ro-id/33bc542c-0486-4ede-8084-e214390cb615/resources/5f488eeb-2534-465b-bbe1-c8912ebeb230
type: BibliographicResource
type: Resource
type: MediaObject
date created: 2022-03-22 01:07:56.542332+00:00
date modified: 2022-03-22 01:07:56.792761+00:00
license: no-permission
name: https://doi.org/10.5194/esd-10-569-2019
sd date published: 2022-03-22 01:07:56.542332+00:00

NorESM1-Happi slab ocean climate sensitivity experiments
type: Dataset
type: Resource
type: MediaObject
bibliographic citation: Debernard, J. B. (2020).NorESM1-Happi slab ocean climate sensitivity experiments [Data set]. Norstore. https://doi.org/10.11582/2020.00014
rights holder: Jens Boldingh Debernard
type: Model
date created: 2020-03-20 00:00:00
date modified: 2022-03-22 01:08:00.261265+00:00
description: These experiments are used to calculate the climate sensitivity of NorESM1-Happi with a slab ocean configuration. Consists of a 1850 control simulation with slab ocean q-fluxes derived from the NorESM1-Happi fully coupled 1850 control. A 2xCO2 experiment, and a 4xCO2 experiment. Those two experiments use the same q-flux field as the control simualtion, so the only forcing that is changed is the CO2 concentration in the atmosphere. Data description: case = N1Happi_som_1850_02; N1Happi_som_1850_2XCO2_02; N1Happi_som_1850_4XCO2_01; Source = CAM ; Variables = P0:reference pressure ; lat:latitude ; lon:longitude ; slat:staggered latitude ; slon:staggered longitude ; w_stag:staggered latitude weights ; lev:hybrid level at midpoints (1000*(A+B)) ; ilev:hybrid level at interfaces (1000*(A+B)) ; isccp_prs:Mean ISCCP pressure ; isccp_tau:Mean ISCCP optical depth ; isccp_prstau:Mean pressure (mb).mean optical depth (unitless)/1000 ; time:time ; time_bnds:time interval endpoints ; ntrm:spectral truncation parameter M ; ntrn:spectral truncation parameter N ; ntrk:spectral truncation parameter K ; ndbase:base day ; nsbase:seconds of base day ; nbdate:base date (YYYYMMDD) ; nbsec:seconds of base date ; mdt:timestep ; nlon:number of longitudes ; wnummax:cutoff Fourier wavenumber ; hyai:hybrid A coefficient at layer interfaces ; hybi:hybrid B coefficient at layer interfaces ; hyam:hybrid A coefficient at layer midpoints ; hybm:hybrid B coefficient at layer midpoints ; gw:gauss weights ; ndcur:current day (from base day) ; nscur:current seconds of current day ; date:current date (YYYYMMDD) ; co2vmr:co2 volume mixing ratio ; ch4vmr:ch4 volume mixing ratio ; n2ovmr:n2o volume mixing ratio ; f11vmr:f11 volume mixing ratio ; f12vmr:f12 volume mixing ratio ; sol_tsi:total solar irradiance ; datesec:current seconds of current date ; nsteph:current timestep ; ABSVIS:Aerosol absorptive optical depth at 0.35-0.64um ; AEROD_v:Total Aerosol Optical Depth in visible band ; AKCXS:Scheme excess ae…
license: no-permission
sd date published: 2020-03-20 00:00:00
maintainer: Jens Boldingh Debernard

Geo H.
type: Agent

Jens Boldingh Debernard
type: Agent

sig
has algorithm: RSA
signed by: RoCrateBot