Kuroda (2002), Dynamical response to the solar cycle, J. Geophys. Res., 107 (D24), 4749, doi: 10.1029/2002JD002224.Kodera, K., and Kuroda, Y.: 2002, `Dynamical response to the solar cycle', J. Geophys. Res. 107, art. No. 2224....
Transfer of the solar signal from the stratosphere to the troposphere: Northern winter. The atmospheric response to the solar cycle has been previously investigated with the Freie Universit盲t Berlin Climate Middle Atmosphere Model (FUB-CMAM) ... K Matthes,Y Kuroda,K Kodera,... 被引量: 318发...
Atmospheric transport and dispersion models (ATDMs) are widely used to study and forecast pollution events. In the frame of the “Effect of Megacities on the transport and transformation of pollutants on the regional to global scales” (EMeRGe) project, ATDM forecasts were carried out to identify...
This finding indicates that the positive carbon cycle feedback from increased fire provides a substantial contribution to the overall climate–carbon-cycle feedback on centennial timescales. Although the feedback estimates from palaeo- and satellite-era data are in agreement, this is likely fortuitous ...
In spite of the extensive studies on ENSO mechanisms, the influence of MC on the characteristics of ENSO life cycle remains unclear. Our coupled model experiments reveal that the absence of the MC land contributes to a strong ENSO asymmetry and a weakened nonlinear atmospheric response to the ...
In a nonlinear system, linear superposition fails and a system need not change proportionally to the change in a variable. If you turn your volume control up two units and the volume increases tenfold, this would be an example of a nonlinear response. View chapterExplore book Low-Dimensional ...
select article Energy management set-up to exploit the flexibility potential of a multi-unit residential apartment building in a cold climate region Research articleFull text access Energy management set-up to exploit the flexibility potential of a multi-unit residential apartment building in a cold ...
When assessing impacts of MHW characteristics, it is important to clearly differentiate between the long-term externally forced warming trend from changes in internal variability. Therefore, the decision to use a fixed or moving climatological baseline to identify MHW events should be made based on th...
As a response to the westerlies increase, mixed layer is deepened mainly around the latitude 60°S circle (Figure 9d). Figure 9 Open in figure viewerPowerPoint Zonal wind stress from CFSR reanalysis (a), the difference between Mod_cp and F09 (b); zonal wind speed of atmosphere bottom ...
On the annual cycle of upper-ocean circulation in the eastern Equatorial Pacific Journal of Physical Oceanography, 27 H. Sverdrup(1947) Wind-Driven Currents in a Baroclinic Ocean; with Application to the Equatorial Currents of the Eastern Pacific. ...