1993

  1. [Barlow et al. 1993]
    Extreme modes of NAO index are reflected in isotopic signals
    Ref. de [Appenzeller et al. 1998a]

  2. [Berz 1993]
    Changes in storminess have a significant impact on a variety of socio economic relevant activities and risks. An economic segment obviously sensitive to changes in the risk of wind related damages is the insurance industry ([Berz 1993,Berz and Conrad 1994]). Other relevant aspects are related to ocean waves and storm surges, and therir impat on off shore activities shiping and coastal structures.
    Ref. de [von Storch and Weisse 2007]

  3. [Deser and Blackmon 1993]
    SST and AT EOFs related in reverse order with decadal and biennal variability
    Western Atlantic pattern seems to force SST anomalies through advection of cold dry air and stronger than normal winds and alteration of fluxes of latent and sensible heat.
    In NAO negative phase pattern positive SST anomalies over the Gulf stream current are related to encreased wind downstream.
    Posible liks to thermohaline circulation: Intensified oceanic thermohaline circulation is associated with surface warming at high latitudes of the North Atlantic Ocean and an intensification of poleward shift of Gulf Stream. The atmospheric response is weakening of wind system (negative NAO). Relationship with periods of cooling and warming proposed. Relationship between ice in the Labrador Sea and
    Interesante por relacions con temperatura, NAO, corriente do Golfo, termohalina, etc.

  4. [Downton and Katz 1993]
    Test for inhomogeneities in variance using resampling techniques
    Homogenization, variance, tests, bootstrap

  5. [Grootes et al. 1993]
    RECENT results1,2 from the Greenland Ice-core Project (GRIP) Summit ice core suggest that the climate in Greenland has been remarkably stable during the Holocene, but was extremely unstable for the time period represented by the rest of the core, spanning the last two glaciations and the intervening Eemian inter-glacial. Here we present the complete oxygen isotope record for the Greenland Ice Sheet Project 2 (GISP2) core, drilled 28 km west of the GRIP core. We observe large, rapid climate fluctuations throughout the last glacial period, which closely match those reported for the GRIP core. However, in the bottom 10
    GISP, GRIP Greenland Ice Cores

  6. [Hoyt and Schatten 1993] Reconstruction of solar irradiance
    Solar irradiance, last millennium

  7. [Lara and Villalba 1993]
    Reconstruction of temperatures for southern chile. No evidence of climate change.
    Paleoclimate, temperature reconstructions, tree ring.

  8. [Rhoades and Salinger 1993]
    Homogeneity test dependent on metadata. Methods for estimating the effect of known site changes on temperature and preciptation in USA.
    Homogeneization

  9. [von Storch et al. 1993]
    Applies CCA model of [Zorita et al. 1992] to GCM control and scenario outputs. The reliability of GCM results depends on the spatial scale.
    GCM simulations, downscaling, CCA.

  10. [Valero et al. 1993]
    Analysis of time series of monthly precipitation totals for Almeria, San Javier and Alicante stations. Spectral and crossespectral analysis. Q-Q plots.
    Desertification. Southwestern Iberia. Precipitation. Annual cycle.

  11. [Young 1993]
    Inhomogeneities in monthly SLP time series. Aplication to Darwin
    Interpolation, inhomogeneities