Signs of Change? An Analysis of Taiwan's December 2009 Local Elections
Under special circumstances created by a government decision to partly merge and upgrade six counties and county-level cities to special municipality status, local elections took place on December 5, 2009 in areas covering less than half of Taiwan's population. The results are generally seen as an important, though small, victory for the opposition Democratic Progressive Party (DPP). The ruling Kuomintang (KMT) (Guomindang), however, has remained in a stable position, while the DPP still has a long way to go towards a comeback.
Faction versus Ideology: Mobilization Strategies in Taiwan's Elections
On 2 December 1989, voters on Taiwan cast ballots to elect national legislators (lifaweiyuan), provincial and city representatives (sheng/shiyiyuari) and county executives (xianzhang). Though the Nationalist Party (KMT) received 59 per cent of the overall vote, the election was widely viewed as a surprising success for the fledgling opposition party, the Democratic Progressive Party (DPP), since the KMT had polled over 70 per cent of the vote in all previous elections. James Soong, Secretary-General of the KMT, announced after an emergency meeting of the shocked KMT leadership, “We calmly accept an upset.”
Observations of nearshore infragravity waves: Seaward and shoreward propagating components
[1] The variation of seaward and shoreward infragravity energy fluxes across the shoaling and surf zones of a gently sloping sandy beach is estimated from field observations and related to forcing by groups of sea and swell, dissipation, and shoreline reflection. Data from collocated pressure and velocity sensors deployed between 1 and 6 m water depth are combined, using the assumption of cross-shore propagation, to decompose the infragravity wave field into shoreward and seaward propagating components. Seaward of the surf zone, shoreward propagating infragravity waves are amplified by nonlinear interactions with groups of sea and swell, and the shoreward infragravity energy flux increases in the onshore direction. In the surf zone, nonlinear phase coupling between infragravity waves and groups of sea and swell decreases, as does the shoreward infragravity energy flux, consistent with the cessation of nonlinear forcing and the increased importance of infragravity wave dissipation. Seaward propagating infragravity waves are not phase coupled to incident wave groups, and their energy levels suggest strong infragravity wave reflection near the shoreline. The cross-shore variation of the seaward energy flux is weaker than that of the shoreward flux, resulting in cross-shore variation of the squared infragravity reflection coefficient (ratio of seaward to shoreward energy flux) between about 0.4 and 1.5.