meteorology – storm events. knowledge of precipitation amounts and patterns plan drainage...

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Meteorology – Storm Events

Knowledge of Precipitation Amounts and Patterns

• Plan drainage structures– Size temporary

culverts to handle storm events during period of operations

– Size permanent drainage structure to handle 100 year storms

Know Precipitation Amounts and Patterns

• Time operations– Expose soil during dry periods

if possible– Establish vegetative cover as

soon as possible– Use native vegetation

whenever possible

What’s Wrong?

Become familiar with precipitation

patterns• Sources of data

– NOAA

– NWS

– State climatologist• Usually at Land Grant

University

• Vast amount of data available on line

Ochocos Mountains of Central Oregon

National Climatic Data Center

http://www.ncdc.noaa.gov/oa/ncdc.html

National Weather Servicehttp://www.weather.gov/view/national.php?thumbs=on

National Oceanic and Atmospheric Administration's   

 National Weather Service   

Indiana State Climatologist

http://www.agry.purdue.edu/climate/

Variation in Precipitation

• Random• Seasonal• Proximity to water

body (lake affect)• Prevailing winds

with moisture• Topographic

Seasonal Variation

Indiana Total Precipitation

0

1

2

3

4

5

Jan.

Mar.

May

July

Sep.

Nov.

Month

Inch

es

NC

SC

State

Proximity to Water Body

Prevailing Winds

Topographic Affect

• Rising air cools• Dew point reached• Water vapor

condenses to form clouds

• Precipitation may occur

• Cloud patterns induced by passage of air current over mountains

• Precipitation concentrated on windward side of mountain, and mountain top

• Tends to be rain shadow on leeward side

• Fidalgo Island in rain shadow of the Olympic Mountains.

• Rainforests with up to 200 inches of precipitation on the west side.

• Rain shadow area northeast of the Peninsula with only one-half (20 inches) of the normal rainfall for the rest of the region.

Avg. Monthly Rainfall 1931-1998

02468101214161820

Month

Inch

es

Clearwater 118.5”

Coupeville 21.14”

Puget Sound Area, Washington

Storm Events, 1st Qtr.

Daily Precipitation, Bedford, IN, 1998

00.20.40.60.81

1/1/99

1/8/99

1/15/99

1/22/99

1/29/99

2/5/99

2/12/99

2/19/99

2/26/99

3/5/99

3/12/99

3/19/99

3/26/99

Inch

es

Storm Events, 2nd Qtr.

Daily Precipitation, 1998, Bedford, IN

012345

4/1/99

4/8/99

4/15/99

4/22/99

4/29/99

5/6/99

5/13/99

5/20/99

5/27/99

6/3/99

6/10/99

6/17/99

6/24/99

Inch

es

Storm Events, 3rd Qtr.

Daily Precipitation, 1998, Bedford, IN

00.20.40.60.81

1.2

7/1/99

7/8/99

7/15/99

7/22/99

7/29/99

8/5/99

8/12/99

8/19/99

8/26/99

9/2/99

9/9/99

9/16/99

9/23/99

9/30/99

Inch

es

Storm Events, 4th Qtr.

Daily Precipitation, 1998, Bedford, IN

00.51

1.52

2.5

10/1/99

10/8/99

10/15/99

10/22/99

10/29/99

11/5/99

11/12/99

11/19/99

11/26/99

12/3/99

12/10/99

12/17/99

12/24/99

12/31/99

Inch

es

Monroe County Airport, April 15-16, 1998

15th 0953 .03

1053 .26

1158 .00

1253 .01

1353 .0

1453 .04

1553 .0

1953 .14

2053 .12

2153 .10

2253 .36

2353 .17

16th 0053 .32

0153 .22

0253 .25

0353 .08

Hourly Precipitation

0

0.1

0.2

0.3

0.4

Series1

Some Basic Hydrologic Concepts

Weirs are used to measure volume of water flowing past a point.

What Happens to Precipitation?

• Hydrologic cycleP = RO + ET + S,

Where,• P ≡ precipitation

• RO ≡ runoff

• ET ≡ evapotranspiration

• S ≡ storage

Evapotranspiration

• Loss of water from a given area during a specified time by evaporation from the soil surface and by transpiration from the plants.

• Supports plant life• Reduces water yield

Runoff Provides Major Benefits RO = P – ET

Moose Creek, Clearfield County, PA (WLH)

Where does runoff go to?

• RO = CI + SRO + SSF + BF, – where,

• CI ≡ channel interception• SRO ≡ surface run off • SSF ≡ subsurface flow• BF ≡ base flow

Where does runoff go to?

– CI ≡ channel interception• Precipitation falling directly into

channel

Susquehanna River, Clearfield, PA, (WLH)

Where does runoff go to?– SRO ≡ surface runoff or overland flow

• Precipitation not infiltrating soil

Sheet erosion of cropland resulting from surface runoff

Source: http://www.agric.gov.ab.ca/agdex/500/72000003.html

Where does runoff go to?

– SSF ≡ subsurface flow, or interflow• Infiltrating precipitation intercepted by hardpan or

bedrock before entering groundwater pool

Where does runoff go to?– BF ≡ base flow or ground water flow

• Precipitation entering water table

Research results come from experimental watersheds such as:

What We’ll Look At

• Erosion– Impacts of

• Roads• Harvests

• Water flows– Storm events– Storage

• Water yield– Amount– Timing Montgemory Reservoir, Clearfield, PA, WLH

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