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Figures

Figure 1: Scheme of stratospheric mass transport processes (J=jetstream).
\begin{figure} \centerline{\hbox{ \psfig{figure=trans.ps,width=140mm,height=80mm}}} \end{figure}

Figure 2: Scheme of extended ray path in a spherical layer. A ray from zenith angle $\Theta $ passes through a layer of thickness $d$ with a bottom height $h$ above ground. The ray path is given by $a_{2}-a_{1}$.
\begin{figure} \centerline{\hbox{ \psfig{figure=strweg.ps,width=120mm,height=50mm}}} \end{figure}

Figure 3: Comparison of volcanic induced aerosol optical depth ($AOD$) time series for four equal area boxes. Top panel: northern hemisphere extra-tropics, second panel: northern hemisphere tropics, third panel: southern hemisphere tropics, bottom panel: southern hemisphere extra-tropics. Solid lines: this paper; dashed lines: Stothers (1996); dotted lines: Sato et al. (1993, 1995)
\begin{figure} \centerline{\hbox{ \psfig{figure=aodver6.ps,width=160mm,height=160mm}}} \end{figure}

Figure 4: Comparison of globally averaged volcanic $AOD$ time series. Solid line: this paper; dashed line: Stothers (1996); dotted line: Sato (1995)
\begin{figure} \centerline{\hbox{ \psfig{figure=aodver3.ps,width=160mm,height=90mm}}} \end{figure}

Figure 5: Comparison of volcanic radiative forcing time series ($W/m^{2}$) for four equal area latitude belts. Top panel: northern hemisphere extra-tropics, second panel: northern hemisphere tropics, third panel: southern hemisphere tropics, bottom panel: southern hemisphere extra-tropics. Solid lines: this paper; dashed lines: after Stothers (1996) and Lacis et al. (1992); dotted lines: after Sato (1995) and Lacis et al. (1992).
\begin{figure} \centerline{\hbox{ \psfig{figure=heatver6.ps,width=160mm,height=160mm}}} \end{figure}

Figure 6: Comparison of globally averaged volcanic radiative forcing time series ($W/m^{2}$). Solid line: this paper; dashed line: after Stothers (1996) and Lacis et al. (1992); dotted lines: after Sato (1995) and Lacis et al. (1992).
\begin{figure} \centerline{\hbox{ \psfig{figure=heatver3.ps,width=160mm,height=90mm}}} \end{figure}

Figure 7: Comparison of volcanic radiative forcing time series ($W/m^{2}$) for four equal area boxes. Top panel: northern hemisphere extra-tropics, second panel: northern hemisphere tropics, third panel: southern hemisphere tropics, bottom panel: southern hemisphere extra-tropics. Solid lines: eruption occured in January; Dashed lines: eruption occured in July.
\begin{figure} \centerline{\hbox{ \psfig{figure=hv15.ps,width=160mm,height=160mm}}} \end{figure}

Figure 8: Estimated volcanic radiative forcing time series ($W/m^{2}$) for four equal area boxes since 1500. Top panel: northern hemisphere extra-tropics, second panel: northern hemisphere tropics, third panel: southern hemisphere tropics, bottom panel: southern hemisphere extra-tropics.
\begin{figure} \centerline{\hbox{ \psfig{figure=heatlang.ps,width=160mm,height=160mm}}} \end{figure}

Figure 9: Comparison of spatio-temporal $AOD$ patterns from January 1982 until June 1986 (a) from Sato (1995), and (b) this paper.
\begin{figure} \centerline{\hbox{ \psfig{figure=elcaod.ps,width=160mm,height=90mm}}} \end{figure}

Figure 10: Spatio-temporal pattern of volcanic forcing ($W/m^{2}$) from January 1982 until June 1986.
\begin{figure} \centerline{\hbox{ \psfig{figure=elch3d.ps,width=100mm,height=100mm}}} \end{figure}

Figure 11: Comparison of spatio-temporal $AOD$ patterns from January 1912 until June 1916 (a) from Sato (1995), (b) from Stothers (1996), and (c) this paper.
\begin{figure} \centerline{\hbox{ \psfig{figure=katmai.ps,width=160mm,height=160mm}}} \end{figure}

Figure 12: Estimates of spatio-temporal patterns of (a) $AOD$, and (b) radiative forcing ($W/m^{2}$) from January 79 A.D. until June 83 A.D.
\begin{figure} \centerline{\hbox{ \psfig{figure=vesuv.ps,width=160mm,height=90mm}}} \end{figure}

next up previous
Next: About this document ... Up: Parameterization of Spatio-temporal Patterns Previous: Tables
ich 2000-01-20