Physically, since all of the DSR shift factors for a temperature of 17 °C, with 22 °C as the reference, are below 1, this lengthens the timescale of the data and implies that the same amount of creep occurs for two cases, when appropriately scaled: (1) a shorter time scale with a warmer temperature, and (2) a longer time scale with a cooler temperature.
Physically, since all of the DSR shift factors for a temperature of 17 °C, with 22 °C as the reference, are below 1, this lengthens the timescale of the data and implies that the same amount of creep occurs for two cases, when appropriately scaled: (1) a shorter time scale with a warmer temperature, and (2) a longer time scale with a cooler temperature.
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