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. Grieser , C. Beck , B. Rudolf , and F. Rubel , 2006 : World Map of the Köppen-Geiger climate classification updated . Meteor. Z. , 15 , 259 – 263 , https://doi.org/10.1127/0941-2948/2006/0130 . 10.1127/0941-2948/2006/0130 Krogh , S. A. , and J. W. Pomeroy , 2018 : Recent changes to the hydrological cycle of an Arctic basin at the tundra–taiga transition . Hydrol. Earth Syst. Sci. , 22 , 3993 – 4014 , https://doi.org/10.5194/hess-22-3993-2018 . 10.5194/hess-22-3993-2018 Krogh
. Grieser , C. Beck , B. Rudolf , and F. Rubel , 2006 : World Map of the Köppen-Geiger climate classification updated . Meteor. Z. , 15 , 259 – 263 , https://doi.org/10.1127/0941-2948/2006/0130 . 10.1127/0941-2948/2006/0130 Krogh , S. A. , and J. W. Pomeroy , 2018 : Recent changes to the hydrological cycle of an Arctic basin at the tundra–taiga transition . Hydrol. Earth Syst. Sci. , 22 , 3993 – 4014 , https://doi.org/10.5194/hess-22-3993-2018 . 10.5194/hess-22-3993-2018 Krogh
, pixel-level brightness temperatures of a snowfall profile over snow-covered tundra shall be closer to those of snowfall over grasslands than those of rainfall over woody savannas. Figure 15 provides evidence for acceptance of such a hypothesis showing that the nearest neighbors in vector space of TB values can isolate physically consistent rainfall profiles. These results simply demonstrate that the uncertainty of such a matching approach can be higher over land than oceans. Building on such a
, pixel-level brightness temperatures of a snowfall profile over snow-covered tundra shall be closer to those of snowfall over grasslands than those of rainfall over woody savannas. Figure 15 provides evidence for acceptance of such a hypothesis showing that the nearest neighbors in vector space of TB values can isolate physically consistent rainfall profiles. These results simply demonstrate that the uncertainty of such a matching approach can be higher over land than oceans. Building on such a
