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This is a measure of water inflow by precipitation, with high values corresponding to a high likelihood of flooding owing to depletion of water storage capability in the floodplain and reduced water outflow (due to ground saturation and high river stages). This dataset shows Projected average number in consecutive wet days in a given year relative to the 2041–2060 period. Texas Tech University Climate Center/University of Illinois Urbana-Champaign; Source contact: Ian Scott-Fleming, Department of Electrical and computer Engineering, Texas Tech University. |
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This is a measure of water inflow by precipitation, with high values corresponding to a high likelihood of flooding owing to depletion of water storage capability in the floodplain and reduced water outflow (due to ground saturation and high river stages). This dataset shows Projected average number in consecutive wet days in a given year relative to the 2041–2060 period. Texas Tech University Climate Center/University of Illinois Urbana-Champaign; Source contact: Ian Scott-Fleming, Department of Electrical and computer Engineering, Texas Tech University. |
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<DIV STYLE="text-align:Left;"><P><SPAN>This is a measure of water inflow by precipitation, with high values corresponding to a high likelihood of flooding owing to depletion of water storage capability in the floodplain and reduced water outflow (due to ground saturation and high river stages). This dataset shows Projected average number in consecutive wet days in a given year relative to the 2041–2060 period. Texas Tech University Climate Center/University of Illinois Urbana-Champaign; Source contact: Ian Scott-Fleming, Department of Electrical and computer Engineering, Texas Tech University.</SPAN></P></DIV> |
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maxcwd_41_60 |
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en-US |
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150000000 |
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