mapping temperature across complex terrain · 2009. 4. 28. · mapping temperature across complex...
TRANSCRIPT
![Page 1: Mapping Temperature across Complex Terrain · 2009. 4. 28. · Mapping Temperature across Complex Terrain Jessica Lundquist 1, Nick Pepin. 2, Phil Mote. 3. 1. Assistant Professor,](https://reader035.vdocument.in/reader035/viewer/2022071515/6136c1e60ad5d206764839cb/html5/thumbnails/1.jpg)
Mapping Temperature across Complex Terrain
Jessica Lundquist1, Nick Pepin2, Phil Mote31Assistant Professor, Civil and Environmental Engineering, University of Washington
2 Lecturer, Department of Geography, University of Portsmouth3Washington State Climatologist, Climate Impacts Group, U. Washington
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• World overview: temperatures at higher elevations
• Implications for snowmelt and the rain-snow line
• Temperature inversions
• Mapping cold-air pools
• Temperature Toolbox webpage
Talk outline
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Trends from 1084 stations ranging in elevation from 500-4700 m across the globe (Pepin and Lundquist, in press, and Pepin and Seidel, 2005)
Tropical Stations Extratropical Stations
elevation
Tem
pera
ture
tren
d (o C
per d
ecad
e)
mean
0
-0.5
-1
0.5
1
0
-0.5
-1
0.5
1
elevation
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• Measurements are sparse at higher elevations.
• Measurements may be unrepresentative of surrounding topography.
•. This can have huge implications for modeling ecology, snowmelt, and the rain-snow line.
What accounts for huge scatter?
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Streamflow simulations depend on knowing high elevation
temperatures.
0
10
20
30
40
50
60
70
80
10 11 12 1 2 3 4 5 6 7 8 9
Month
Stre
amflo
w (C
MS)
OBSSIM
winter spring
Snohomish River in Western Washington, courtesy of Alan Hamlet
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Streamflow simulations depend on knowing high elevation
temperatures.
0
10
20
30
40
50
60
70
80
10 11 12 1 2 3 4 5 6 7 8 9
Month
Stre
amflo
w (C
MS)
OBSSIM
winter spring
Modeled mountain temp is too cold = too much snow falls = underestimates winter rain runoff & overestimates spring snowmelt
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Area contributing to runoff (through rain or melting snow) depends on how temperature
decreases with altitude
+15+15°°CC Sea level00°°CC
elev
atio
nDepends on lapse rate:
Average decrease = 6.5°C per km
But could range from 3 to 9.8 °C per km
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A biased valley temperature sensor could also misrepresent the elevation where snow melts.
+15+15°°CC Sea level00°°CC
elev
atio
n
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Temperature inversions and cold- air pools are common in mountain valleys, which is where many temperature sensors are located.
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Inversions occur during high pressure, when large-scale winds are weak, and
local topography controls mountain weather.
alpine sites
valley sites
From Lundquist and Cayan, 2007
Inversions are common in valleys near Mt. Rainier, making the standard lapse rate often wrong.
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Fortunately, we know how mountain winds and cold air pools work and can map them with a DEM (Example, Loch Vale, Rocky Mountain National Park, Colorado)
1) Density-driven drainage
2) Pressure-gradient-driven drainage
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1) At night, longwave radiation cools air adjacent to the surface.
2) Cold air is denser than warm air, and flows down hill and down valley.
3) Therefore, cold air can collect in flat valley bottoms and local depressions.
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iButton Location
Loch Vale, Rocky Mtn NP
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Primary Mode of Variability is
cold-air pooling:
Explains 72% of the Variance
Positive Weight
Negative Weight
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Mapping likely cold-air pools using a digital elevation map (DEM).
Flat slope
Local depression ConcaveLund
quis
t et a
l. 20
08 (s
ubm
itted
to J
GR)
Impo
rtan
t fac
tors
iden
tifie
d in
fore
stry
lite
ratu
re.
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This method identifies flat valley bottoms (white), but only one of two
identified is cold-air pool.
Andrew’s Meadow = flat bottom without cold-air pooling
Loch Vale = correctly identified cold-air pool
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Topographic Amplification Factor• Represents how much more a valley
cools at night compared to a flat plain
From
mou
ntai
n m
eteo
rolo
gy li
tera
ture
,W
hite
man
, 199
0; M
cKee
and
O’N
eal 1
989
Energy lost to space = Volume x ΔT
W
H
(TAF)
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Topographic Amplification Factor• Represents how much more a valley
cools at night compared to a flat plain
Whi
tem
an, 1
990;
McK
ee a
nd O
’Nea
l 198
9
Smaller enclosed volume = cools more = bigger TAF
W
H
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Topographic Amplification Factor
• Areas that cool more have local higher pressure.
• Winds flow from high to low pressure.
• Places where TAF decreases down- valley drain, and where TAF
increases, cold air pools
Whi
tem
an, 1
990;
McK
ee a
nd O
’Nea
l 198
9
W
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TAF decreases through Andrew’s Meadow, so it drains.
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Main Loch Vale: TAF increases, cold air pools.
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Applied mapping algorithm to study areas in the Rocky Mountains, Pyrenees, and Sierra Nevada, and can predict areas
of CAP with over 80% accuracy.
Lundquist et al. 2008, submitted to JGR
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Using CAP-mapping to interpolate station temperature data results in an average of 1oC improvement over standard interpolation techniques.
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Valley Fog, Guipuzcoa, Basque Country, Spain from wallpaperme.com
http://faculty.washington.edu/jdlund/TemperatureToolbox/
Find: Links to all the papers discussed here.
Directions for deploying temperature sensors in trees.
Code for CAP-mapping algorithm and empirical orthogonal function (EOF) based method of identifying modes of temperature variability.
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Conclusions
1)
Mountains poorly sampled: samples may not represent surrounding topography
2)
Temperature patterns strongly influenced by large-scale weather patterns and by local topography
3)
GIS-based mapping can help improve how we model temperature variations across complex terrain
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The Temperature Sensors:Dallas Semiconductor Maxim iButton DS-1922L
- 17.35 mm diameter
- 5.89 mm thickness
- temperature range:
-35°C to +85°C
- records temperature at user-defined rate:
8192 8-bit readings (0.5°C resolution) or 4096 16-bit readings (0.0625°C resolution)
at intervals ranging from:
1s to 273hr
- 512 bytes for application info
- 64 bytes for calibration data
0.5°C resolution+Sample once per hour=
11 months of data
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Tuolumne i-buttons
Different radiation shielding from trees
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The Pacific Northwest has
taller trees than most of
the Rockies or the Sierra
Jeremy Littel
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Biology Professor Janneke Hille Ris Lambers
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Eset Alemu
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Rocky Mountain Field Study:
Dave Clow (Colorado USGS), Mark Losleben (Colorado Mountain Research Station(MRS)),
Kurt Chowanski (MRS), Todd Ackerman(MRS), Jen Kelley, Hollings Scholarship Program
Caitlin Rochford
CIRES Innovative Research Fellowship
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Acknowledgements
Yosemite Field Study: Brian Huggett (NPS), Dan Cayan (SIO), Mike Dettinger (USGS), Heidi Roop (Mt. Holyoke), Jim Roche (NPS), Frank Gehrke (CA DWR), Kelly Redmond (WRCC), Canon Research Fellowship, NSF RoadNET program, CIRES Postdoctoral Fellowship