15
From Drought to Flood FMA Annual Meeting 2017 Dr. Michael Anderson, State Climatologist

From Drought to Flood

  • Upload
    others

  • View
    3

  • Download
    0

Embed Size (px)

Citation preview

Page 1: From Drought to Flood

From Drought to Flood

FMA Annual Meeting 2017

Dr. Michael Anderson, State Climatologist

Page 2: From Drought to Flood

0

20

40

60

80

100

120

140

1899

1903

1907

1911

1915

1919

1923

1927

1931

1935

1939

1943

1947

1951

1955

1959

1963

1967

1971

1975

1979

1983

1987

1991

1995

1999

2003

2007

2011

2015

California Statewide 4-yearPrecipitation Sum4-yearPrecipitation Sum

Year 4-year sum2015 62.21920 63.01926 63.31931 64.41934 65.1

Lowest Totals

Average:85.9 inches

Page 3: From Drought to Flood

0

10

20

30

40

50

60

70

80

50 51 52 53 54 55 56 57 58

Annu

al P

reci

pita

tion

(inch

es)

Annual Average Temperature (deg F)

Climate Division 2 (Sacramento Basin) – Calendar Year Data

1895-2000 21st Century POR Average

2

2013

2014

2015

2016

Page 4: From Drought to Flood

0

50

100

150

200

250

20 25 30 35April

1 S

now

pack

Per

cent

of A

vera

geFr

om C

alifo

rnia

Coo

pera

tive

Snow

Sur

veys

Sierra Winter (DJF) Average Minimum Temperature (degrees Fahrenheit)

SierraRegion

9 Years Below 50%

Snowpack and Winter Temperatures of the Sierra Nevada

2013 20142015

2016

2017

Page 5: From Drought to Flood

Distribution of Landfalling Atmospheric Rivers on the U.S. West Coast (From 1 Oct 2016 to 12 April 2017)

Ralph/CW3E AR Strength Scale• Weak: IVT=250–500 kg m–1 s–1

• Moderate: IVT=500–750 kg m–1 s–1

• Strong: IVT=750–1000 kg m–1 s–1

• Extreme: IVT>1000 kg m–1 s–1

AR Strength AR Count*

Weak 12

Moderate 21

Strong 13

Extreme 3

• 49 Atmospheric Rivers have made landfall on the West Coast thus far during the 2017 water year (1 Oct. – 12 April 2017)

• This is much greater than normal • 1/3 of the landfalling ARs have been “strong” or “extreme”

*Radiosondes at Bodega Bay, CA indicated the 10–11 Jan AR was strong (noted as moderate based on GFS analysis data) and 7–8 Feb AR was extreme (noted as strong)

By F.M. Ralph, B. Kawzenuk, C. Hecht, J. KalanskyCenter for Western Weather and Water ExtremesScripps Institution of Oceanography

Water year 2017 AR landfall

locations through 11 April 2017

Location of landfall represents position where AR was strongest at landfall . Many ARs move down the coast over time. This map does not show these areas.

Page 6: From Drought to Flood

Magnitude DurationBetween

Clustering

FreezingElevation

From Ben Hatchett, WRCC, UNR

12”

18”

26”31”5750’

EventDuration

Page 7: From Drought to Flood

Seasonal Outlook for Water Year 2018

Page 8: From Drought to Flood

Storm Track changes

Flooding & water supply

MJO/Tropical Convection ENSO

Polar Processes

Key Phenomena Affecting California Water Supply/Flooding:

Easterly Wave

CyclogensisL

The size, number, and strength of atmospheric river events (ARs) result from the alignment of key

physical processes operating on different space and time scales that will change with climate change

Page 9: From Drought to Flood

Circulation Patterns of Note

Page 10: From Drought to Flood

IRI/CPC Pacific Niño 3.4 SST Model Outlook

Figure provided by the International Research Institute (IRI) for Climate and Society (updated 18 August 2017).

Most models and the multi-model averages predict ENSO-Neutral through the remainder of the year and into early 2018.

From Climate Prediction Center’s ENSO Diagnostic Discussion

Page 11: From Drought to Flood

U. S. Seasonal Outlooks

Precipitation Temperature

September – November 2017

The seasonal outlooks combine the effects of long-term trends, soil moisture, and, when appropriate, ENSO.

Page 12: From Drought to Flood
Page 13: From Drought to Flood
Page 14: From Drought to Flood
Page 15: From Drought to Flood

Signposts for the Seasons

• Fall – Heat and/or decaying tropicals?

• Winter – Will the circulation align for a cluster of ARs once or twice?

• Spring – Early shutdown?

• Can you have a flood and a below average water year?