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Summary:
The Legates Surface and Ship Observation of Precipitation Data Set was
produced by Dr. David Legates, University of Oklahoma, and Dr. Cort
Willmott, University of Delaware. The data set represents a global
climatology of mean monthly precipitation based upon traditional
land-based rain gauge measurements and shipboard measurements. The
rain gauge measurements were collected from existing sources, coding
errors were corrected and redundant station information removed. The
result of these steps provided a data base of 24,635 spatially
independent terrestrial station records and 2223 oceanic grid records.
A procedure for correcting the gauge-induced biases was implemented to
remove the systematic errors associated with traditional rain gauge
collection methods. The corrected monthly precipitation measurements
were then interpolated to a 0.5 degree latitude by 0.5 degree longitude
grid using a spherically based interpolation procedure.
This climatology is largely representative of the 60-year period from
1920 to 1980; with greater weight given to the more recent (data-rich)
years.
Table of Contents:
- Legates Surface and Ship Observation of Precipitation
- The Legates surface and ship observation of precipitation data set
consists of a global climatology of monthly mean precipitation values,
using traditional land-based gauge measurements and shipboard estimates.
- The objective of this data set is to provide an improved
climatology data set that is based upon a spatially dense network of
terrestrial rain gauge station measurements and accurate estimates of oceanic
precipitation that have been corrected for major biases inherent in
gauge collection procedures.
- This global data set contains monthly mean precipitation.
- This information is not available at this time.
- Jaeger Monthly Mean Global Precipitation
- Dr. David R. Legates
- Department of Geography
- College of Geosciences
- University of Oklahoma
- Norman, OK 73019
and
- Dr. Cort J. Wilmont
- Department of Geography
- Center for Climatic Research
- University of Delaware
- Newark, DE 19176
- Mean Seasonal and Spatial Variability in Gauge Corrected,
Global Precipitation
- Please direct all queries to Goddard Space Flight Center (GSFC) DAAC Help
Desk.
- DAAC Help Desk:
The DAAC help desk also provides additional information on the Goddard DAAC
system capabilities, and other supported datasets. The Help Desk can be reached
at:
- EOS Distributed Active Archive Center (DAAC)
- Code 610.2
- NASA Goddard Space Flight Center
- Greenbelt, Maryland 20771
- Internet:daacuso@daac.gsfc.nasa.gov
- 301-614-5224 (voice)
- 301-614-5268 (fax)
Data are compiled from terrestrial precipitation gauge measurements in
their traditional setting (elevated above the ground and possibly with
a gauge shield) and the indirect oceanic precipitation estimation
technique of Dorman and Bourke. This procedure estimates precipitation
using a statistically-derived relationship between gauge catch and the
current weather code of the surface synoptic record taken on board
ships (see references). Long-term monthly mean values were compiled
from these measurements and estimates. Biases (underestimates)
resulting from the effect of the precipitation gauge were subsequently
estimated and removed from these monthly mean precipitation data by
taking into account local variations in gauge type, height of the gauge
above the ground, air temperature, wind speed, and general regional
sheltering.
- Ground and aboard ships.
- Meteorological Stations and Ships.
- This information is not available at this time.
- Precipitation, predominantly rain and snow.
- Rain gauges data collection methods vary. The collection of
precipitation measurements occurs on a periodic basis.
The rain gauges used for the terrestrial gauge
measurements were used in their traditional setting (elevated above the ground and possibly with
a gauge shield). The data is based upon 24,635 independent stations
which provided a dense network in the industrialized countries of North
America, Europe, and East Asia. Station distribution in the arid,
mountainous, and polar regions, however, are less dense.
- The manufacturer of the rain gauges varies.
- This information is not available at this time.
- This information is not available at this time.
- This information is not available at this time.
- This information is not available at this time.
Global archives of monthly precipitation compiled by Wernstedt (1972),
Willmott, et al. (1981) and the National Center for Atmospheric
Research (Spangler and Jenne, 1984) provided most of the terrestrial data for this
climatology data set. To improve the spatial resolution in the above mentioned regions,
monthly averages were obtained from an additional 208 stations in
Australia, New Guinea, and Indonesia, 584 stations in China and the Far
East, and ten stations in Antarctica. Five stations in the Sahara also
provided monthly precipitation averages.
- There are no data notes for this data set.
- There are no field notes for this data set.
-
The data set is global in coverage. The data is based upon 24,635 independent stations
which provided a dense network in the industrialized countries of North
America, Europe, and East Asia. Station distribution in the arid,
mountainous, and polar regions, however, are less dense.
-
- The spatial resolution of the data is 0.5 degree latitude by 0.5 degree longitude grids.
- No projection was used to process the data since the data are directly related to
geographic areas.
- The data are on a 0.5 x 0.5 degree grid for the area from 90N to 90S and 180W to 180E.
In order to achieve a dense spatial resolution, virtually
all station records from the existing sources were used even though they
were based upon differing time periods. Most of the data was observed
between 1920 and 1980, therefore, this climatology is largely
representative of that 60 year period. The data file spans the period from 1920 to 1980.
- This climatology contains monthly mean precipitation for each month of the 60 year period.
- The temporal resolution is monthly.
- The key parameter is precipitation.
Precipitation - Any or all forms of liquid or solid water particles that fall from the
atmosphere and reach the surface of the Earth. It includes drizzle, rain, snow, snow
pellets, snow grains, ice crystals, ice pellets, and hail. Precipitation is also defined as a
measurement of the quantity, expressed in centimeters or milliliters of liquid water
depth, of the water substance that has fallen at a given location in a specified amount of
time.
- The monthly mean precipitation data are in millimeters.
- Rain gauges.
- The range of the data is from 0 to approximately 5500 mm.
90.0 -180.0 15 11 18 14 11 11 27 30 43 23 21 17 241
89.5 -180.0 15 10 18 13 11 11 27 30 42 22 19 16 234
89.0 -180.0 12 5 16 10 10 8 27 28 38 18 13 11 196
88.5 -180.0 9 2 15 8 8 5 26 25 35 14 7 7 161
88.0 -180.0 7 2 15 8 7 4 26 25 35 14 5 6 154
87.5 -180.0 6 2 15 8 6 4 25 24 35 14 4 6 149
- A general description of data granularity as it applies
to the IMS appears in the
EOSDIS Glossary.
- The data for the entire period of record is contained in a
single file. This file is in UNIX compress format of the size 5.4 Megabyte
(uncompressed size is approximately 21 Megabyte
- The monthly mean
precipitation total
is stored in a 361 by 721 element array. The data is in ASCII format. The name of the file is: legates.cor.Z
The rain gauge measurements were collected from existing
sources, coding errors were corrected and redundant station information
removed. The result of these steps provided a data base of 24,635
spatially independent terrestrial station records and 2223 oceanic grid
records. A procedure for correcting the gauge-induced basis was
implemented to remove the systematic errors associated with traditional
rain gauge collection methods.
For this data set, the oceanic precipitation is estimated using the method of Dorman and
Bourke (1979). Their method was derived from a technique proposed by J. S. Sawyer and later
refined by Tucker (1961).
The method of Tucker has been determined to be suitable for estimating
oceanic preipitation only in the mid-latitudes. In the tropics, the
increased rainfall intensity reduced the effectiveness of Tucker's
method. Dorman and Bourke (1978) also observed that the error was
systematic and highly correlated to air temperature. They developed a
set of regression equations, one for each month, to remove the error
from Tucker's estimates. Dorman and Bourke used shipboard observations
from 1950 to 1972 to estimate average monthly precipitation for the
Pacific and Atlantic Oceans north of 30 degrees South at the vertices of
a 2 degree latitude by 5 degree longitude lattice. These estimates were
used in the development of this data set.
Dorman and Bourke could not obtain reliable estimates for the Indian and
Southern Ocean south of 30 degrees South. For these regions, this data
set used the estimates of Jaeger's (1983) global precipitation
climatology. Jeager used a variation of the typical precipitation
frequency approach to generate his estimates.
The estimates of Jaeger and those of Dorman and Bourke are not
commensurate. Systematic differences between the two approaches had to
be resolved before the estimates could be used for this data set.
Jaeger's estimates were converted into values compariable with Dorman
and Bourke by applying multiple linear regression to data from the
Atlantic and Pacific Oceans north of 30 degrees South.
- This information is not available at this time.
- This information is not available at this time.
- This information is not available at this time.
- Terrestrial and oceanic precipitation.
- This information is not available at this time.
- This information is not available at this time.
- This information is not available at this time.
- This information is not available at this time.
- This information is not available at this time.
- This information is not available at this time.
- This information is not available at this time.
- This information is not available at this time.
- This information is not available at this time.
- This information is not available at this time.
- This information is not available at this time.
-
This data set can be used to verify general circulation model
(GCM)
prognostications of the seasonal precipitation cycle and GCM dynamics, as ground truth
for evaluating and calibrating precipitation estimates obtained from
radars and satellites, and as a basis for evaluating climate change.
- The processing of this data set is complete.
- No software is provided with this data set. However, a brief sample Fortran code that provides
information on how to read the data set format is included in the documentation distributed
with the data set.
- This information is not applicable for this data set.
- Goddard Space Flight Center DAAC User Services.
- GSFC Distributed Active Archive Center
- This data set is available via several ways: by contacting
the GSFC DAAC User Services, by accessing the DAAC/EOSDIS Archive Search and Order Utilities,
the WWW interface, or Anonymous FTP.
- The DAAC User Services or Help Desk also provides additional information on the Goddard DAAC
system capabilities, and other supported datasets. The Help Desk can be
reached at:
EOS Distributed Active Archive Center (DAAC)
Code 610.2
NASA Goddard Space Flight Center
Greenbelt, Maryland 20771
Internet:daacuso@daac.gsfc.nasa.gov
301-614-5224 (voice)
301-614-5268 (fax)
DAAC SEARCH AND ORDER SERVICES:
- These datasets are available from the Goddard DAAC.
ANONYMOUS FTP:
The legates precipitation data set resides on DAAC
anonymous FTP. The data files may be accessed from this document,
Legates Surface and Ship Observation of Precipitation
- or directly via FTP:
- ftp disc1.gsfc.nasa.gov
- login: anonymous
- password: < your email address >
- cd data/hydrology/precip/legates
- The GSFC DAAC will continue to archive and distribute updates
received from the data producer. The Goddard DAAC plans to periodically check with the data
producer regarding the data set revisions.
- Data sets are available on anonymous ftp.
Dorman, C. E. and Bourke, R. H., 1979: Precipitation over the Pacific
Ocean, 30S to 60N. Monthly Weather Review, Vol 107, 896-910.
Dorman, C. E. and Bourke, R. H., 1981: Precipitation over the Atlantic
Ocean, 30S to 70N. Monthly Weather Review, Vol 109, 554-563.
Jaeger, L., 1983: Monthly and Areal Patterns of Mean Global
Precipitation. in Street-Perrott, A. et al. (eds) Variations in
the Global Water Budget, D. Reidel, Dordrecht, p. 129.
Legates, D.R., 1987: A Climatology of Global Precipitation. Publications
in Climatology, Vol. 40(1), 84 pp.
Legates, D.R. and C.J. Wilmott, 1990: Mean Seasonal and Spatial
Variability in Gauge-Corrected, Global Precipitation. International
Journal of Climatology, Vol. 10, 111-127.
Spangler, W. M. L and Jenne, R. L., 1984: World Monthly Surface Station
Climatology. National Center for Atmospheric Research. 14 pp.
Wernstedt, F. L., 1972: World Climatic Data. Climatic Data Press.
Willmott, C. J., Mather, J. R., and Rowe, C. M., 1981: Average Monthly
and Annual Surface Air Temperature and Precipitation Data for the World.
Part 1: The Eastern Hemisphere. Part 2: The Western Hemisphere.
Publications in Climatology, Vol 34, 395 pp and 378 pp.
- See the EOSDIS Glossary for a more
general listing of terms related to the Earth Observing System
project.
-
See the EOSDIS Acronyms for a more
general listing of terms related to the Earth Observing System
project.
-
Uniform Resource Locator
- August 1, 1996
- August 1, 1996
- Not available at this time.
- Not available at this time.
- Suraiya Ahmad (ahmad@daac.gsfc.nasa.gov)
-
http://disc.sci.gsfc.nasa.gov/DATASET_DOCS/legates_rain_gauge_dataset.html
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