While the local,
seasonal climate forcing by the Milankovitch cycles is large (of the order 30 W / m2), the net forcing provided by Milankovitch is close to zero in the global mean, requiring other radiative terms (like albedo or greenhouse gas anomalies) to force global - mean temperature change.
Not exact matches
I have a special interest in plankton interactions with the physical environment; looking for quantitative and mechanistic links to current structure, water mass shifts,
seasonal cycles, interannual variability,
climate - related signals, wind
forcing, etc..
These orbital variations, which can be calculated from astronomical laws (Berger, 1978),
force climate variations by changing the
seasonal and latitudinal distribution of solar radiation (Chapter 6).
The community [studying]
seasonal and longer
climate variability was (and still is) dominated by the ocean community and especially a decade ago [the El Niño Southern Oscillation] ENSO was the only boundary
forcing that anyone was paying attention to.
Although the primary driver of glacial — interglacial cycles lies in the
seasonal and latitudinal distribution of incoming solar energy driven by changes in the geometry of the Earth's orbit around the Sun («orbital
forcing»), reconstructions and simulations together show that the full magnitude of glacial — interglacial temperature and ice volume changes can not be explained without accounting for changes in atmospheric CO2 content and the associated
climate feedbacks.
Climate modelers are very thankful for the existence of the
seasonal cycle, for providing such a beautiful data set with which we can test a models quantitative response to a well - defined change in external
forcing.
The U.S. military seems interested in
climate variations / change on timescales from
seasonal to scales out to about 30 years, a period over which natural
climate variability could very well swamp anthropogenically
forced climate change.
A top - down
climate effect that shows long - term drift (and may also be out of phase with the bottom - up solar
forcing) would change the spatial response patterns and would mean that
climate - chemistry models that have sufficient resolution in the stratosphere would become very important for making accurate regional /
seasonal climate predictions.
What I actually said — and have always said — is that if the net of * all * feedbacks in the
climate system is negative, then a mere
seasonal and spatial reorganisation of TSI under orbital
forcing would not be capable of terminating glacials.
Halloran, A., 2012: Growing Uncertainties:
Climate change is
forcing farmers in the Northeast to rethink their
seasonal strategies.
CAS = Commission for Atmospheric Sciences CMDP =
Climate Metrics and Diagnostic Panel CMIP = Coupled Model Intercomparison Project DAOS = Working Group on Data Assimilation and Observing Systems GASS = Global Atmospheric System Studies panel GEWEX = Global Energy and Water Cycle Experiment GLASS = Global Land - Atmosphere System Studies panel GOV = Global Ocean Data Assimilation Experiment (GODAE) Ocean View JWGFVR = Joint Working Group on Forecast Verification Research MJO - TF = Madden - Julian Oscillation Task
Force PDEF = Working Group on Predictability, Dynamics and Ensemble Forecasting PPP = Polar Prediction Project QPF = Quantitative precipitation forecast S2S = Subseasonal to
Seasonal Prediction Project SPARC = Stratospheric Processes and their Role in
Climate TC = Tropical cyclone WCRP = World
Climate Research Programme WCRP Grand Science Challenges •
Climate Extremes • Clouds, Circulation and
Climate Sensitivity • Melting Ice and Global Consequences • Regional Sea - Ice Change and Coastal Impacts • Water Availability WCRP JSC = Joint Scientific Committee WGCM = Working Group on Coupled Modelling WGSIP = Working Group on Subseasonal to Interdecadal Prediction WWRP = World Weather Research Programme YOPP = Year of Polar Prediction
«There is evidence of an emerging pattern of
climate response to
forcing by greenhouse gases and sulfate aerosols... from the geographical,
seasonal and vertical patterns of temperature change... These results point toward a human influence on global
climate.»
Crespin, E., Goosse, H., Fichefet, T., Mairesse, A. & Sallaz - Damaz, Y. Arctic
climate over the past millennium: Annual and
seasonal responses to external
forcings.
Comparing the influences on the Last Interglacial
climate with those assumed in future
climate projections is problematic owing to fundamental differences, especially orbital
forcing,
seasonal warming, and greenhouse gas concentrations.
The new low ice cover state has been sampled predominantly in summer - autumn and
seasonal forcing combined with internal
climate variability are likely responsible for triggering recent transitions between the two ice cover states.
I came to think of solar radiation as being the ultimate (and only) external
forcing of the
climate system, which, except for the orbital
seasonal changes and the 11 - year sunspot cycle, has been essentially constant over the past several decades of precision solar irradiance monitoring.
A recent study by C10 analysed a number of different
climate variables in a set of SMEs of HadCM3 (Gordon et al. 2000, atmosphere — ocean coupled version of HadSM3) from the point of view of global - scale model errors and
climate change
forcings and feedbacks, and compared them with variables derived from the CMIP3 MME. Knutti et al. (2006) examined another SME based on the HadSM3 model, and found a strong relationship between the magnitude of the
seasonal cycle and
climate sensitivity, which was not reproduced in the CMIP3 ensemble.
Recent analyses using the CCM3
climate model (Govindasamy and Caldeira, 2000) suggest, however, that a 1.7 % decrease in solar luminosity would closely counterbalance a doubling of CO2 at the regional and
seasonal scale (in addition to that at the global and annual scale) despite differences in radiative
forcing patterns.»