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I suddenly realized that I’d accepted my introduction as “Didi” without a moment’s hesitation. That was my new name and it seemed to fit and sit comfortably in my head. Victoria left and I was caught up in the blur of waitressing. I carried drinks on a tray, rushed back to the kitchen to refill it and then back out to the guests. I had no time to think or stop to reflect on my situation. It was too busy and I had to really concentrate in carrying the drinks tray without spilling drinks or dropping it. The guests were spread all over the house. There were several formal lounge rooms and some guests where in the TV room and other lounge rooms upstairs. Fortunately I didn’t have to serve upstairs. With my very short dress, I would have been totally exposed from underneath if I had to walk up the stairs. I caught a few fleeting glimpses of Susan (remember my wife?) as I was serving. She seemed to be having a great time and always had a bevy of guys around her. She was totally. " exclaimed Jo. "If you can "time" it forward, can you "time" it back? Say, to the very beginning of this last ice melt. I'd like to know why the melt started." I knew you'd get me in trouble if I presented this "map"," complained She/It/He/Whatever.Jo explained, "There are those who say during ice ages the continental landmass expands. Because so much of the oceans' water is turned to ice, sea level is lowered, this uncovers more land, the climate becomes more seasonal, and probably most importantly, the global climate tends to cool off even more. This is largely because continental masses tend to reflect the Sun's energy back to space, while large bodies of water tend to absorb the Sun's energy. Also, landmasses at the poles permit the growth of permanent ice sheets, which, because they are white, reflect even more energy back to space. The formation of ice on the continents lowers sea level, which exposes more land, which further cools the Earth, forming more ice, and so on, and so.
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