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AUTHOR'S INTRODUCTION: More than twenty-five years ago while researching the fourth Saint-Germain book, Path of the Eclipse, I ran across references to the Year of the Yellow Snow, sometimes called the Year of the Dark Sun, in Western reckoning A.D. 535-36, which was characterized by catastrophic drops in temperature, crop failures, and famine throughout Asia and Europe, with disruption of trade and movements of populations resulting from these losses—just the sort of event to set the speculative juices, flowing, but not the object of my research, nor the period with which I was dealing, promising though it appeared. Then, about ten years ago, other researchers did some serious scholarship on those disastrous events and tried to determine the cause of what turned out to be a worldwide famine and, after considering a number of different scenarios from meteor collisions to a mini-ice age—which indeed occurred—at last identified the probable source of the trouble as an eruption of that all-time bad-boy volcano, Krakatoa; this eruption was more overwhelming than many of its others, for, according to records in Indonesia, this eruption broke Sumatra off from Java—Krakatoa is at the hinge position of those two islands—and opened the Sundra Strait to a deep-water sea passage instead of only the shallowest-draft boats, which it had been for centuries. The eruption occurred in late February or early March of A.D. 535, and its explosion was heard all the way to Beijing. It had been heralded by many months of regional instability, earthquakes, and drastic variations in ocean temperatures in and around what was becoming the Sundra Strait, making the shipping lanes more treacherous than they had been in the past. Many ships' captains reported dangerous sailing in and around Indonesia, and over time, merchant ships avoided the region. ¶ In April, following the eruption, the ash from the volcano had spread all around the world, and disaster followed after it, impacting global weather patterns and lowering the average temperatures sufficiently to keep crops from growing in most of Asia and Europe, as well as large portions of Africa and Americas. Although every part of the world was affected, there were regions that bore more of the brunt of the tragedy than others. Many of the nomadic people of the Central Asian Steppes were driven out of their traditional grazing lands when their herds began to die because of lack of food as the grasslands became arid plains, and their struggle to find new pastureland was made much more difficult by the impact of the colder weather; the significant westward migration from Central Asia began as an attempt to find grass for their herds. In China and Tibet, the snow that continued to fall all the way into June and July was yellow due to the high levels of sulfur in the upper atmosphere. Closer to the eruption site, actual flakes of sulfur fell from the sky, burning people, animals, and fields alike and contaminating wells, springs, and rivers; the devastation of the Indonesian Islands was calamitous, with tens of thousands of people killed in tsunamis spawned by the eruption, by gaseous emanations, and by sulfur contamination, records of which still exist in the royal archives of the Srivijava Empire, which comprised most of modern Indonesia. For months afterward, the remains of humans, animals, trees, sea-life, and buildings washed up on the shores of what are now Indonesia, the Malay Peninsula, the Philippines, China, and India.
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