unstable, dri and water cycling ronald stewart mcgill university

21
UNSTABLE, DRI UNSTABLE, DRI and Water Cycling and Water Cycling Ronald Stewart McGill University

Upload: lillian-williamson

Post on 22-Jan-2016

227 views

Category:

Documents


0 download

TRANSCRIPT

Page 1: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

UNSTABLE, DRI UNSTABLE, DRI and Water Cyclingand Water Cycling

Ronald StewartMcGill University

Page 2: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

Specific Objectives of Presentation

• To briefly review DRI and some of its science

• Comment on interactions with UNSTABLE

Page 3: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

Prairie Drought

Page 4: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

CONCERNS

There are many concerns associated with drought but many of these can be summarized under two broad categories

• Will there be a drought?decadelseasonal‘now’

• How do we best prepare for and cope with drought?

many perspectives

Page 5: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

WATER AND ENERGY CYCLING

Drought is an aberration in theWater and energy cycle

Page 6: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

0

5

10

15

20

25

30

35

40

45

50F

RA

CT

ION

AL

OC

CU

RR

EN

CE

OF

CL

OU

D F

OR

EA

CH

OF

TH

E

FO

UR

CO

ND

ITIO

NS

00-

23 L

ST

(%

)Extreme Drought

Drought

Non-drought

Extreme Wet

CLEAR FEW SCATTERED BROKEN OVERCAST

Page 7: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

0

2

4

6

8

10

12

14

16

18

OC

CU

RR

EN

CE

OF

SP

EC

IFIC

TY

PE

OF

C

ON

VE

CT

IVE

CL

OU

D 0

0-23

LS

T (

%)

Extreme Drought

Drought

Non-drought

Extreme Wet

CUMULUS CUMULUS FRACTUS

TOWERING CUMULUS

CUMULONIMBUS

Page 8: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

0

500

1000

1500

2000

2500

3000

3500

4000

4500

5000

0 2 4 6 8 10 12 14 16 18 20 22

HOUR (LST)

CE

ILIN

G (

m)

Page 9: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

DRI Objective• To better understand and contribute to the

better prediction of drought …

• Focus mainly but not exclusively on the

recent 1999-2005 Prairiedrought

Page 10: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University
Page 11: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

DEUTERIUM IN WATER VAPOUR

550-800 hPa layer

Tropospheric Emission Spectrometer: Aqua satellite

Page 12: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

Days with precipitationCalgary

• The fraction of days receiving any amount of precipitation:

Climatology (1895-2004): 40%

Drought (1999-2004): 46%

Sub-Drought (2001-2002): 43%

Page 13: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

30.8

21.3

15.0

9.6

6.34.6 3.7

1.9 1.5 1.20.4 1.0 0.4 0.5 0.5 0.4 0.5 0.2 0.2

0.0

5.0

10.0

15.0

20.0

25.0

30.0

35.0

40.0

Precipitation Amount Category (mm)

% o

f T

ota

l P

rec

ipit

ati

on

0.0

10.0

20.0

30.0

40.0

50.0

60.0

70.0

80.0

90.0

100.0

Cu

mu

lati

ve

% (

of

tota

l p

rec

ipit

ati

on

)

% Tot. Precip

Cumulative %

33.2

26.7

21.8

8.3

0.0

10.0

0.0

5.0

10.0

15.0

20.0

25.0

30.0

35.0

40.0

Precipitation Amount Category (mm)

% o

f T

ota

l Pre

cip

ita

tio

n

0.0

10.0

20.0

30.0

40.0

50.0

60.0

70.0

80.0

90.0

100.0

Cu

mu

lati

ve

% (

of

tota

l pre

cip

ita

tio

n)

% Tot. Precip

Cumul %

Climatology

Low precipitation events: 52% of total

Sub-drought 2001-2002

Low precipitation events: 60% of total

Daily Precipitation AmountsCalgary Low precipitation event:

< 10 mm

Page 14: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

What factors led to the ≤10 mm events?

Possibilities include

• Loss due to evaporation/sublimation• Short-lived weather systems• Change in character of clouds• Fast moving weather systems• …

Page 15: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

RADAR PROFILES1 June 2002: Calgary

• Scattered stratiform rain early

• Late in the day there is evidence of water aloft (~5 km)

• This appears to be high-level moisture as a precursor to the rainy pattern on the following day

Page 16: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

VIRGA

Courtesy of Barrie Bonsal

Page 17: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

VEGETATION

July 11-20, 2002

NDVI

NDVI: Normalized DifferenceVegetation Index

Healthy vegetation

Page 18: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

UNSTABLE

Sub-objectives include …

to better understand, resolve, and quantify:

• spatial extent, depth and temporal evolution of water vapour in the atmospheric boundary layer

• Mesoscale effects on thunderstorms• effects of variable surface• …

Page 19: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

DRI and UNSTABLE

• DRIdiverse research expertise (~ 30)datasets (atmosphere, surface …)analysis tools (DAI …)…

• UNSTABLEaspects linked with water cyclingfocused activityobservational and model products…

Page 20: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

CONCLUDING REMARKS

• DRI is concerned with:the science of water cycling

• UNSTABLE is concerned with:overturning of the atmosphere

• DRI and UNSTABLE can benefit from collaboration

Page 21: UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University

And … thank you for your attention