1	TmpMonMn Generic	Temperature minimum pattern in generic hydro regime system	6	
6	TmpMonMax GrdWater	Temperature maximum pattern in groundwater dominated stream	5	
31	FlowMax Glacial run-off_(Puyallup_Nooksack)	Primary source of flow is snow- rainfall (pattern similar to transitional); summer flows buffered by glacial melt (low flows not as severe)	2	
32	FlowMin Rainfall	Primary source of precipitation is rainfall with much less contribution by snow.  Large fall and winter storms produce major increases in flow, continuing on into spring, after which flow declines rapidly to summer lows.	3	
33	FlowMin Transitional	Primary sources of precipitation are both snow and rainfall, though rainfall is the dominant source of flow over much of the year.  Large fall and winter storms produce major increases in flow, followed by lesser, though significant, snow caused runoff in	3	
34	FlowMin Snowfed	Primary source of precipitation is snow. Runoff occurs in the spring and early summer, after which flow declines rapidly to a base level. Note: same pattern as transitional was used - GB.	3	
35	FlowMin Groundwater	Primary source of flow is groundwater - some contribution from rainfall - very stable flow throughout year (Metolius River or spring brook example)	3	
36	Turbidity Groundwater	Primary source of flow is groundwater - some contribution from rainfall - very stable flow throughout year (Metolius River or spring brook example)	8	
37	Turbidity Snowfed	Primary source of precipitation is snow. Runoff occurs in the spring and early summer, after which flow declines rapidly to a base level.	8	
38	Turbidity Transitional	Primary sources of precipitation are both snow and rainfall, though rainfall is the dominant source of flow over much of the year.  Large fall and winter storms produce major increases in flow, followed by lesser, though significant, snow caused runoff in	8	
39	Turbidity Rainfall	Primary source of precipitation is rainfall with much less contribution by snow.  Large fall and winter storms produce major increases in flow, continuing on into spring, after which flow declines rapidly to summer lows.	8	
40	Turb Glacial run-off	Primary source of flow is snow- rainfall (pattern similar to transitional); summer flows buffered by glacial melt (low flows not as severe)	8	
41	FlowMin Glacial run-off	Primary source of flow is groundwater - some contribution from rainfall - very stable flow throughout year (Metolius River or spring brook example)	3	
42	TmpSptVar	Special pattern generated for Lewis	7	
43	TmpSptVar	Special pattern generated for Lewis	7	
44	TmpSptVar	Special pattern generated for Lewis	7	
45	TmpSptVar	Special pattern generated for Lewis	7	
46	TmpSptVar	Special pattern generated for Lewis	7	
7	TmpMonMax Spr SnowMelt	Temperature maximum pattern in spring snowmelt stream	5	
8	TmpMonMax Transitional	Temperature maximum pattern in Rain-on-Snow transitional stream	5	
9	TmpMonMax Rainfall	Temperature maximum pattern in rainfall (Puget Sound lowland) stream	5	
10	TmpMonMax Glacial	Temperature maximum pattern in glacial melt dominated system	5	
11	FlowMax Generic	Flow Pattern for maximum attribute effects - generic hydrologic regime; typical Puget Sound lowland stream (rainfall pattern)	2	
12	FlowMin Generic	Flow Pattern for minimum attribute effects - generic hydrologic regime; typical summer pattern in Puget Sound lowland stream (rainfall pattern)	3	
13	No variation in Attribute	Pattern with no monthly variation	4	
14	Flow Rainfall	Primary source of precipitation is rainfall with much less contribution by snow.  Large fall and winter storms produce major increases in flow, continuing on into spring, after which flow declines rapidly to summer lows.	1	
15	Flow Transitional	Primary sources of precipitation are both snow and rainfall, though rainfall is the dominant source of flow over much of the year.  Large fall and winter storms produce major increases in flow, followed by lesser, though significant, snow caused runoff in	1	
16	Flow Snowfed	Primary source of precipitation is snow. Runoff occurs in the spring and early summer, after which flow declines rapidly to a base level.	1	
17	Flow Groundwater	Primary source of flow is groundwater - some contribution from rainfall - very stable flow throughout year (Metolius River or spring brook example)	1	
18	Flow Glacial run-off	Primary source of flow is snow- rainfall (pattern similar to transitional); summer flows buffered by glacial melt (low flows not as severe)	1	
19	Flow Glacial run-off - moderately regulated	Primary source of flow is snow- rainfall (pattern similar to transitional); summer flows buffered by glacial melt (low flows not as severe); flows moderately regulated by dam	1	
20	Flow Rainfall - moderately regulated	Primary source of precipitation is rainfall with much less contribution by snow.  Large fall and winter storms produce major increases in flow, continuing on into spring, after which flow declines rapidly to summer lows; summer low flow buffered by regula	1	
21	Flow Transitional - moderately regulated	Primary sources of precipitation are both snow and rainfall, though rainfall is the dominant source of flow over much of the year.  Large fall and winter storms produce major increases in flow, followed by lesser, though significant, snow caused runoff in	1	
22	Flow Snowfed - moderately regulated	Primary sources of precipitation is snow.  Runoff occurs in the spring and early summer, after which flow declines rapidly to a base level; summer low flow buffered by regulation and peak spring flows flattened for flood control.	1	
23	Flow Glacial run-off - heavily regulated	Primary source of flow is snow- rainfall (pattern similar to transitional); summer flows buffered by glacial melt (low flows not as severe); flows heavily regulated by dam for flood control and power generation.	1	
24	Flow Rainfall - heavily regulated	Primary source of precipitation is rainfall with much less contribution by snow.  Large fall and winter storms produce major increases in flow, continuing on into spring, after which flow declines rapidly to summer lows; flows heavily regulated by dam for	1	
25	Flow Transitional - heavily regulated	Primary sources of precipitation are both snow and rainfall, though rainfall is the dominant source of flow over much of the year.  Large fall and winter storms produce major increases in flow, followed by lesser, though significant, snow caused runoff in	1	
26	Flow Snowfed - heavily regulated	Primary sources of precipitation is snow.  Runoff occurs in the spring and early summer, after which flow declines rapidly to a base level; flows heavily regulated by dam for flood control and power generation.	1	
27	FlowMax Rainfall - Puget Sound Ecoregion	Primary source of precipitation is rainfall with much less contribution by snow.  Large fall and winter storms produce major increases in flow, continuing on into spring, after which flow declines rapidly to summer lows.	2	
28	FlowMax Transitional_Revised for Dungeness	Primary sources of precipitation are both snow and rainfall, though rainfall is the dominant source of flow over much of the year.  Large fall and winter storms produce major increases in flow, followed by lesser, though significant, snow caused runoff in	2	
29	FlowMax Snowfed	Primary source of precipitation is snow. Runoff occurs in the spring and early summer, after which flow declines rapidly to a base level.	2	
30	FlowMax Groundwater	Primary source of flow is groundwater - some contribution from rainfall - very stable flow throughout year (Metolius River or spring brook example)	2	
