Basic Tools in Meteorology and Climatology René Garreaud .
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Transcript of Basic Tools in Meteorology and Climatology René Garreaud .
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Basic Tools inMeteorology and Climatology
René Garreaudwww.dgf.uchile.cl/rene
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Since pressure always decrease with height, sometimes we use pressure as the vertical coordinate (instead of m ASL). In this case, geopotential height (Z) is a variable. For instance, at the 500 hPa level, Z usually varies between 5300-5600 m.
Atmospheric pressure:Weight of the air column above you
Units: hPa = mb = 100 Pa = 100 * N/m2
p(z) p0exp(-z/H*) ~ 1013*exp(z/8000) [hPa if z in meters], H* = R[T]/g height scale
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Air temperature ~ kinetic energy of air moleculesChanges because heat flux divergence
Radiosonde (p,T,RH,…)with height
Average (time, space) temperature profile of the earth atmosphere. Note and explain the three maxima.
T usually decrease with height (unstable condition)Inversion layers (stable air) where T increase with height
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ff [m/s]dd [°]
streamline
streamline
Local wind
u > 0v > 0
u < 0v < 0u < 0
v < 0
Blowing from….SW
SE
NE
Wind is a vector: magnitude (speed) and blowing direction (° wrt north)Alternatively, zonal (u, west-east) and meridional (v, south-north) components
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Mapa de Observaciones Carta del tiempo
Every day meteorologist have quite a lot of data that need to be synthesized to detect weather patterns. Analysis: Hand-made (old) or objective (computer)
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Isobars: lines of constant pressure at a given level(e.g. sea level pressure chart) and time (snapshot).
High (anticyclones) and Low (cyclones) pressure centers.
HH
L
L
SLP map, October 17 2010
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Isotherms: lines of constant air temperature at a given level(z or p) and time (snapshot).
The temperature field usually decreases poleward and often exhibits elongated bands of strong thermal gradient (baroclinicity) called fronts
T @ 850 hPa (1500 m ASL)October 17, 2010
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Wind @ 300 hPa (9000 m ASL)
Map showing wind vectors (arrows) and wind speed (colors)Note the presence of wind maxima (jet streams)
Jet stream
Mostly zonal flow Mostly meridional flow
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XX: Lines of constant geopotential height at a given pressure levelTrough: relative minimum pressure. Ridge: relative maximum pressure
In both cases “relative” looking at a same latitude
Z @ 300 hPa (9000 m ASL)
Trough
Ridge
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pi1 = pi2 = pi3 pi1 = pi2 = pi3 pi1 > pi2 < pi3
ps1 = ps2 = ps3 ps1 < ps2 > ps3 ps1 < ps2 > ps3
psup
pinf
C
What causes the pressure gradients (or geopotential gradients) in the atmosphere? Case 1: Thermal contrasts.
Combining hydrostatic and ideal gas equations one can show:
Z = RTg-1*log10(pinf/psup)
1. Inicialmente, las tres columnas son identicas2. La columna central se calienta diferencialmente3. Aire en col. más cálida se expande... Aparece gradiente de presión en altura4. Viento diverge, sacando masa de la columna5. Presión cae en superficie...parece gradiente cerca de la superficie6. Viento converge, agregando masa de la columna
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0 km
12 km
L
HL
H
Warmer Cooler
The mass field (pressure) adjust rapidly to the thermal forcingNote that pressure remains unchanged at the level of warming
Eventually, atmospheric circulation will flatten pressure field
Z = RTg-1*log10(pinf/psup)
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We now can reinterpret troughs and ridges seen in the geopotential height in the upper troposphere (e.g., 300 hPa) as tongues of cold air abnormally at low latitudes and warm air abnormally at high latitudes
Geopotential @ 300 hPa (contours)Air temperature averaged between 700 and 400 hPa (colors)
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Trayectoria desdesistema terrestre
t = 0 t = dT
Trayectoria desdesistema inercial
Fh=0Observador
en Tierra
Air will flow from high pressure areas toward low pressure areasEarth rotation, however, complicate things…apparently
Earth rotation introduce an apparent force that deviate air parcels from its expected trajectory. This force is called the Coriolis force and obeys the following rules:
• Acts over moving air and water parcels• Deflects air parcels to the left in the SH (right in the NH)• Its magnitude is zero at the equator and increase to a maximum at the poles.
Partículas flotando sobre superficieparten impulsivamente al ecuador….
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A AA
En el ecuador o enplaneta sin rotación
Muy cerca del ecuador orotación planetaria muy lenta
Lejos del ecuador (>20) para movimientos lentos
¿Como circula el aire en torno a los centros de alta y baja presión (HS)?
B BB
Air will flow from high pressure areas toward low pressure areasEarth rotation, however, complicate things…apparently
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zf
gkp
fkV
y
pfu
x
pfv
Fgpvdt
vd
Fam
g
R
ˆ1ˆ
11
12
Atmospheric dynamics (same for ocean)
Second Newton’s law:
Which in the atmospherebecomes...
Scale analysis for large-scaleflow leads to…
So we can define the geostrophicwind, very close to actual wind in large scale systems
CoriolisPressuregradient Friction
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HL H
Geostrophic wind (close to actual wind) rules of operation (SH):
• Clock-wise around a low, anti-clockwise around a high• Stronger in areas of tight isobars (or geopotential lines)• Not very usefull at low latitudes
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B
A
B
B
B
A
A
Isobaras
¿Porque nos gustan tanto los mapas del tiempo?
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Climate data issues
• Temporal resolution (daily, monthly, yearly)• Temporal coverage and continuity• Quality and QControl• Station data versus gridded products• Spatial context• Multi variable records (T, P, ….)• Data sources• Data formats (ASCII, NC, never Excel!)• Data sharing etiquette
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Surface (land/ocean) Synoptic Stations Met. Observations (T,Td,P,V,…) @ 0, 6, 12, 18 UTC are transmitted in real-time to
WMO and Analysis Centers
From where do we get climate data? Almost all climate data is initially meteorological data, acquired to assist weather nowcast and forecast (especially for aviation)
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Red de Radiosondas (OMM, GTS)
Perfiles verticales (20 km) de T, HR, viento, presión, cada 12 / 24 hr
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All stations (anytime, any length)
Century-long stations (Ti<1905, Tf>1995, missdata<20%)
Precipitation Mean Temperature
Global Historical Climate Network (GHCN)
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Surface and UpperAir Observations
Satellite Products
Assimilationsystem
Gridded Analysis
Griddingmethod
DATA SOURCES AND PRODUCTS
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Table 1. Main features of datasets commonly used in climate studies
Dataset Key referencesInput data -Variables
Spatial resolution -Coverage
Time span -Time resolution
Station GHCN
Peterson and Vose (1997)
Sfc. Obs Precip and SAT
N/A Land only
1850(*) – present Daily and Monthly
GriddedGHCN
Peterson and Vose (1997)
Sfc. Obs Precip and SAT
5° 5° lat-lon Land only
1900 – present Monthly
GriddedUEA-CRU
New et al. 2000Sfc. Obs Precip and SAT
3.75° 2.5° lat-lon Land only
1900 – present Monthly
GriddedUEA-CRU05
Mitchell and Jones (2005)
Sfc. Obs Precip and SAT
0.5° 0.5° lat-lon Land only
1901 – present Monthly
GridddedU. Delware
Legates and Willmott (1999a,b)
Sfc. Obs Precip and SAT
0.5° 0.5° lat-lon Land only
1950 – 1999 Monthly
GriddedSAM-CDC data
Liebmann and Allured (2005)
Sfc. Obs Precip
1° 1° lat-lon South America
1940 – 2006 Daily and Monthly
GriddedCMAP
Xie and Arkin (1987)Sfc. Obs.; Sat. data Precip
2.5° 2.5° lat-lon Global
1979 – present Pentad and Monthly
GriddedGCPC
Adler et al. (2003)Sfc. Obs.; Sat. data Precip
2.5° 2.5° lat-lon Global
1979 – present Monthly
NCEP-NCAR Reanalysis (NNR)
Kalnay et al. 1996Kistler et al. 2001
Sfc. Obs.; UA Obs; Sat. data Pressure, temp., winds, etc.
2.5° 2.5° lat-lon,17 vertical levels Global
1948 – present 6 hr, daily, monthly
ECMWF Reanalysis(ERA-40)
Uppala et al. (2005)Sfc. Obs., UA Obs, Sat. data Pressure, temp., winds, etc.
2.5° 2.5° lat-lon,17 vertical levels Global
1948 – present 6 hr, daily, monthly
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http://www.cdc.noaa.gov
http://www.ncdc.noaa.gov
http://iridl.ldeo.columbia.edu/
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Because analysis are produced in real-time, some data is not assimilated, but it was archived. In the 90’s the NCEP-NCAR (USA) began a major project in which they re-run their assimilation system with all the available data.
The result is the widely used “Reanalysis” data, including many fields (air temperature, wind, pressure) on a regular 2.5°x2.5° lat-lon grid, from 1948 to present every 6 hours (also available daily, monthly and long-term-mean means). Fields are 2- or 3-Dimensional. Preferred data format: NetCDF. Freely available.
Reanalysis?!
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Reanalysis system also includes a meteorological model from which precipitation and other not-observed variables (e.g., vertical motion) are derived.
Reanalysis data is great for studying interannual and higher frequency variability. Interdecadal variability and trends are not so well depicted (we don’t trust much before the 70’s, particularly in the SH).
European Center (ECMWF) did a similar effort (ERA-15 and ERA-40). Higher horizontal resolution (1.25°x1.25°), but harder to get.
Reanalysis