Alfonso Sutera

ORCID: 0000-0002-5700-5967
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About
Contact & Profiles
Research Areas
  • Climate variability and models
  • Meteorological Phenomena and Simulations
  • Oceanographic and Atmospheric Processes
  • Ionosphere and magnetosphere dynamics
  • Hydrology and Drought Analysis
  • Atmospheric Ozone and Climate
  • Geophysics and Gravity Measurements
  • Atmospheric and Environmental Gas Dynamics
  • Advanced Thermodynamics and Statistical Mechanics
  • Ecosystem dynamics and resilience
  • GNSS positioning and interference
  • Solar and Space Plasma Dynamics
  • Geology and Paleoclimatology Research
  • Nonlinear Dynamics and Pattern Formation
  • stochastic dynamics and bifurcation
  • Plant Water Relations and Carbon Dynamics
  • Complex Systems and Time Series Analysis
  • Atmospheric chemistry and aerosols
  • Tree-ring climate responses
  • Climate change impacts on agriculture
  • Geomagnetism and Paleomagnetism Studies
  • Methane Hydrates and Related Phenomena
  • Scientific Research and Discoveries
  • Marine and coastal ecosystems
  • Theoretical and Computational Physics

Sapienza University of Rome
2004-2014

Università di Camerino
1991-1995

Yale University
1986-1991

Saint Joseph's College
1988

Hartford Financial Services (United States)
1981-1986

European Centre for Medium-Range Weather Forecasts
1986

IBM (Italy)
1984-1985

Lesbian, Gay, Bisexual and Transgender Community Center
1981-1982

Institute of Atmospheric Sciences and Climate
1981

It is shown that a dynamical system subject to both periodic forcing and random perturbation may show resonance (peak in the power spectrum) which absent when either or absent.

10.1088/0305-4470/14/11/006 article EN Journal of Physics A Mathematical and General 1981-11-01

An amplification of random perturbations by the interaction non-linearities internal to climatic system with external, orbital forcing is found.This stochastic resonance investigated in a highly simplified, zero-dimensional climate model.It conceivable that this new type might play role explaining lo5 year peak power spectra paleoclimatic records.

10.1111/j.2153-3490.1982.tb01787.x article EN Tellus 1982-02-01

An amplification of random perturbations by the interaction non-linearities internal to climatic system with external, orbital forcing is found. This stochastic resonance investigated in a highly simplified, zero-dimensional climate model. It conceivable that this new type might play role explaining 105 year peak power spectra paleoclimatic records.

10.3402/tellusa.v34i1.10782 article EN Tellus A Dynamic Meteorology and Oceanography 1982-01-01

In this paper we study a one-dimensional, nonlinear stochastic differential equation when small amplitude, long-period forcing is applied. The arises in the theory of climate earth. We find that cooperative effect perturbation and periodic lead to an amplification peak power spectrum, due mechanism call resonance. A heuristic analysis resonance condition presented our analytical findings are confirmed by numerical calculations.

10.1137/0143037 article EN SIAM Journal on Applied Mathematics 1983-06-01

10.1023/a:1024716530289 article EN Water Resources Management 2003-01-01

Abstract. Linear and nonlinear trends of drought wetness are analysed in terms the gridded Standardized Precipitation Index (SPI) determined from monthly precipitation Europe (NCEP/NCAR). In characterizing meteorological hydrological aspects, index is computed on a seasonal bi-annual time scale. Two datasets compared: one 1949 to 1997 other includes update last decade (to February 2009). The following results noted: (i) series area coverage (number grid points above/below severity threshold)...

10.5194/hess-13-1519-2009 article EN cc-by Hydrology and earth system sciences 2009-08-25

Problems related to the identification and monitoring of drought are investigated. In particular, conditions in Italy examined using Standardized Precipitation Index (SPI) on different time scales for August 2000. Historical reconstruction events is also shown particular locations last fifty years. These preliminary applications show interesting results demonstrate that index considered a tool should be used operationally as part national watch system monitor objectively. An example monthly...

10.4401/ag-3549 article EN cc-by Annals of Geophysics 2009-12-18

An amplification of random perturbations by the interaction non-linearities internal to climatic system with external, orbital forcing is found. This stochastic resonance investigated in a highly simplified, zero-dimensional climate model. It conceivable that this new type might play role explaining 10 5 year peak power spectra paleoclimatic records. DOI: 10.1111/j.2153-3490.1982.tb01787.x

10.3402/tellusb.v34i1.14322 article EN cc-by Tellus B 2012-06-13

The statistical properties of a measure planetary-scale wave activity are investigated in 16 winter NMC dataset. probability density distribution the wavenumber 2 to 4 amplitude is found be bimodal, confirming earlier results from smaller significance this result established empirically with simulations. It also shown that bimodality not connected any periodicity time series. Partitioning data based on estimation reveals two flow regimes physical space. One corresponds an amplified pattern...

10.1175/1520-0469(1986)043<3250:otpddo>2.0.co;2 article EN Journal of the Atmospheric Sciences 1986-12-01

Abstract In this paper we address the problem of constructing a minimal model atmospheric circulation able to describe bulk statistical properties general in middle latitudes. After brief reexamination Charney‐DeVore theory multiple equilibria, compare that can be deduced from it with those resulting analysis observations northern hemisphere middle‐latitude at 500 mb. While prediction concerning amplitude waves seems confirmed by presence clear bimodality distribution, find no trace zonal...

10.1002/qj.49711247306 article EN Quarterly Journal of the Royal Meteorological Society 1986-07-01

Based on a more detailed model developed previously, governing possible feedbacks between sea ice extent (η), deep-ocean temperature (θ), and atmospheric carbon dioxide, we have constructed simple, deterministic, dynamical system for η θ that yields stable limit cycle as solution. To make the realistic add random (white noise) forcing explore new response function of amplitude this stochastic forcing. Included in analysis are examples sample time series, phase trajectories, variance spectra,...

10.1175/1520-0469(1981)038<0494:sssoas>2.0.co;2 article EN Journal of the Atmospheric Sciences 1981-03-01

Abstract A very simple energy‐balance equation for the mean surface temperature of planet (Budyko‐type model) is perturbed by a stochastic term, simulating numerous ‘weather’ processes not considered in deterministic feed‐back term. In first instance, symmetrical process with three equilibrium states considered. Using standard methods determination probability density distribution, characteristic time which climate system spends neighbourhood one stable before shifting to other expressed...

10.1002/qj.49710745109 article EN Quarterly Journal of the Royal Meteorological Society 1981-01-01

10.1023/a:1013353822381 article EN Water Resources Management 2001-01-01

The mechanism of stochastic resonance is studied in the case Landau-Ginzburg equation stochastically and periodically perturbed, by taking advantage recent developments on partial differential equations. Analytical expressions are given for computing exit times system to estimate range noise which possible.

10.1088/0305-4470/18/12/022 article EN Journal of Physics A Mathematical and General 1985-08-21

A simplified version of a previously described dynamical model governing global ice mass, atmospheric carbon dioxide, and mean ocean temperature is shown to possess solutions, in realistic parameter range, that can replicate the main features climatic variations implied by full, two million years, Quaternary delta-O-18 record. These include major 'transition' between low-ice delta-O-18, low variance mode before roughly 900 kyr BP high-ice, high (near 100 period) after time present. The...

10.1175/1520-0469(1987)044<0236:tmqcta>2.0.co;2 article EN Journal of the Atmospheric Sciences 1987-01-01

Because of the small net rates energy flow involved in very long-term changes ice mass (10−1 W m−2) it will be impossible to proceed a purely deductive manner develop theory for these changes. An inductive approach necessary-perhaps beg formulated terms multi-component stochastic-dynamical systems equations governing variables and feedbacks thought relevant from qualitative physical reasoning (e.g., "conceptual models"). The output such models should required conform as closely possible all...

10.1175/1520-0469(1984)041<0736:amotif>2.0.co;2 article EN other-oa Journal of the Atmospheric Sciences 1984-03-01

Abstract. Space-time variability of hydrological drought and wetness over Iran is investigated using the National Centers for Environmental Prediction/National Center Atmospheric Research (NCEP/NCAR) reanalysis Global Precipitation Climatology Centre (GPCC) dataset common period 1948–2007. The aim to complement previous studies on detection long-term trends in drought/wetness time series applicability data monitoring Iran. Climate conditions area are assessed through Standardized Index (SPI)...

10.5194/hess-14-1919-2010 article EN cc-by Hydrology and earth system sciences 2010-10-12

The time mean spectral energy and enstrophy budgets for blocking versus nonblocking periods from the winters of 1978–79 1976–77 are calculated. major differences in cases were nonlinear interaction terms. A pronounced upscale cascade kinetic intermediate to planetary-scale wavenumbers during was found. During December 1976, a case Atlantic very similar 1978–79, but quite different persistent, greatly amplified, planetary-wave pattern that followed January February 1977 (as identified by...

10.3402/tellusa.v36i1.11465 article EN Tellus A Dynamic Meteorology and Oceanography 1984-01-01
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