ISCCP-H¶
International Satellite Cloud Climatology Project (ISCCP) H-Series Climate Data Record
Discontinued
No longer updated
The official CDR (v01r00) ends in June 2017. NCEI also offers a separate Interim CDR (ICDR) for July 2017 to December 2018 by FTP and calls it temporary. When checked on 2026-10-13, the files in the NCEI and AWS copies had not changed since May 2021, and no schedule for extending the record has been announced. ISCCP-NG, which is meant to continue the record from the ring of geostationary satellites, is at demonstrator stage: CM SAF released one year (2021) in September 2026.
Successor: None (the follow-on ISCCP-NG is still a demonstrator) — On 2026-09-21 CM SAF released a GEO-ring-based ISCCP-NG demonstrator (year 2021, 0.05°, half-hourly) built from level-1 composites of five geostationary satellites. It is not yet a long-term record, so for cloud climatologies after 2017 consider polar-orbiter records such as CLARA-A3 or PATMOS-x as well.
At a glance¶
| Item | Details |
|---|---|
| Section | Satellite › Clouds & radiation |
| Type | Satellite product |
| Domains | Atmosphere, Remote sensing |
| Provider | NOAA NCEI (CDR Program) / CUNY CREST (W. B. Rossow) / NASA GISS |
| Period | 1983-07 ~ 2017-06 |
| Coverage | Global |
| Horizontal resolution | Full HGG, HGH and HGM use a 1° equal-area grid (the number of longitude cells varies with latitude, from 3 at the poles to 360 at the equator); HXG uses a 0.1° equal-angle grid; HXS is about 0.1° in satellite projection (binary). Basic HGG, HGH and HGM are remapped to a 360 × 180 1° equal-angle (latitude-longitude) grid. |
| Vertical resolution | Cloud types defined by cloud-top pressure and optical thickness (18 VIS/IR types, 3 IR-only types) and distributions over pressure bins |
| Temporal resolution | HGG and HXG are 3-hourly instantaneous values (00, 03, …, 21 UTC); HGH is a monthly mean for each of these eight times; HGM is the equally weighted mean of the eight HGH fields. |
| Update frequency | No longer updated (CDR through 2017-06, interim ICDR through 2018-12) |
| Licence | NOAA CDR — publicly available with no restrictions on use; credit to NCEI and the developers and citation of the DOI requested |
| Account required | No |
Note on period: The official CDR covers 1983-07-01 to 2017-06-30 (NCEI metadata; the last Basic HGM file on AWS is June 2017). An interim ICDR made the same way fills July 2017 to December 2018, and NCEI says it will stay available only until the final CDR for that period is released.
How to read the resolution
- Horizontal resolution lists both the native model grid and the grid you download, as given in the official documentation. The same dataset can come on different grids from different providers or products, so check the grid of your downloaded file.
- Grid spacing is not the effective resolution. A provided grid that is finer than the native one carries no extra information.
- Intervals and whether a value is instantaneous, mean or accumulated differ between variables — see 'Available variables' below.
- The 'provided resolution' in lists and the comparison table is a simplified km/degree value for quick comparison. Use this page for exact values.
Overview¶
ISCCP-H is a global cloud climate data record from 1983 onward, built by combining visible and infrared imagery from the world's geostationary weather satellites with NOAA and MetOp polar orbiters (AVHRR). Every three hours it provides cloud amount, cloud-top pressure and temperature, optical thickness, water path and cloud type on a 1° grid, making it nearly the only long record that resolves the diurnal cycle of clouds. It is the third generation, replacing ISCCP-D, and comes as a Full version for specialists and a simpler CF-compliant Basic version.
What changes with the successor¶
ISCCP-D → ISCCP-H¶
Transition: 2017-06
The third ISCCP generation, rebuilding ISCCP-D (produced at NASA GISS through 2009) with new pixel sampling, grids and calibration. It is a generation change within this page, so it is described here.
| Aspect | ISCCP-D | ISCCP-H |
|---|---|---|
| Input pixel sampling | Stage B3 data, about 30 km and 3-hourly | B1U data, about 10 km and 3-hourly (polar-orbiter data also sampled to about 10 km) |
| Gridded product resolution | D1 and D2 on a 280 km equal-area grid (2.5° equivalent) | HGG, HGH and HGM on a 1° equal-area grid; HXG on a 0.1° equal-angle grid |
| Calibration | ISCCP-D calibration | VIS anchor chained from NOAA-9 (through 2009) to NOAA-18 (after); IR gain error for NOAA-15 and later AVHRRs and the post-2001 AVHRR KLM calibration error corrected |
| Products | D1 (3-hourly), D2 (monthly) and others | HXS, HXG, HGS, HGG, HGH and HGM, plus the CF-compliant ISCCP-Basic subset |
| File format | Binary (NCEI still takes orders for D in binary only) | netCDF-4 for every product except HXS |
| Period | 1983-07 to 2009-12 | 1983-07 to 2017-06 (interim ICDR 2017-07 to 2018-12) |
Things to watch when switching
- Do not mix ISCCP-D climatologies or trends with H results. The resolution and calibration differ, so cloud amount differs even over the same region.
- H keeps the cloud retrieval algorithm largely unchanged, so NCEI notes that the biases known from D (viewing-angle and satellite-change effects) carry over to H.
Sources: Young et al. (2018), ESSD — ISCCP H-Series CDR product · NCEI — International Satellite Cloud Climatology Project
Available variables¶
Names and units are from the ISCCP-Basic HGM files (NCEI THREDDS aggregation). In the Full version the same names hold 8-bit counts, and in Full HGG cloud amount is stored as pixel counts (n_cloudy/n_total).
Time-stamp convention — instantaneous, mean or accumulated? — click to show
HGG (3-hourly grid) collects instantaneous observations at each UTC time (00, 03, …, 21). HGH averages each of those times over the month, and HGM averages the eight HGH times with equal weight to give the monthly mean. All times are UTC, not local time.
- Optical thickness (TAU) and water path (WP) come only from daytime VIS/IR retrievals (cosine of solar zenith angle at least 0.2). Night-time values in HGG are filled from adjacent daytime values, and the fill is recorded in
fill_type. - Full-version values are stored as 8-bit counts from 0 to 254, with 255 as missing. Convert them with the lookup tables in each file (for example
pretab,tmptab,tautab,wpatab). The Basic version stores decoded physical values with CF attributes. - In the Basic HGM aggregation the time units are 'hours since 1983-07-15 00:00:00.000 UTC' and
cell_methodsis 'area: mean time: mean within days time: mean over days' (NCEI THREDDS attributes). - Where geostationary coverage is missing and over the poles, polar orbiters pass only a few times a day, so many 3-hourly values are not direct observations. Check
satcodesandsatnamesfor the satellites that contributed.
Source: ISCCP Data Users Guide v5.0 (NCEI) + ISCCP-Basic HGM THREDDS attributes
instantaneous mean accumulated maximum minimum static — instantaneous: value at the time stamp · mean/accumulated/maximum/minimum: over the indicated interval · static: does not change with time
Monthly mean cloud properties (Basic HGM)¶
| Variable | Short name | Units | Time convention | Notes |
|---|---|---|---|---|
| Cloud amount | cldamt |
percent | month mean | |
| IR-only cloud amount | cldamt_ir |
percent | month mean | |
| Cloud amount by cloud type (18 types) | cldamt_types |
percent | month mean | |
| Cloud-top pressure | pc |
hPa | month mean | |
| Cloud-top temperature | tc |
K | month mean | |
| Cloud optical thickness | tau |
1 | month mean | From daytime retrievals only; radiatively weighted average of liquid and ice clouds combined |
| Cloud water path | wp |
- | month mean | The file's units attribute says 'cm', while the users guide describes water path in g m-2. Check the units before use. |
| Snow/ice cover fraction | snoice |
percent | month mean |
3-hourly grid (Basic HGG)¶
| Variable | Short name | Units | Time convention | Notes |
|---|---|---|---|---|
| Cloud amount, cloud-top pressure and temperature, optical thickness, water path | cldamt, pc, tc, tau, wp |
- | instantaneous | Observations at each of 00, 03, …, 21 UTC; night-time tau and wp are filled from daytime values |
| Cloud amount by cloud type | cldamt_types, cldamt_irtypes |
- | instantaneous | In Basic HGG these are pixel counts divided by n_total |
The full variable list is in the official documentation.
How to get the data¶
- NCEI direct download (Full and Basic) — HTTPS directory
- Full HGM and HGH and Basic HGG, HGH and HGM are downloadable. Full HGG, HXG and HXS are large and are ordered through ncei.sat.info@noaa.gov.
- NCEI THREDDS (ISCCP-H Basic aggregations) — THREDDS / OPeNDAP / NCSS
- Basic HGG, HGH and HGM are aggregated into single time series (Best Time Series) that can be subset remotely.
- AWS open bucket (noaa-cdr-cloud-properties-isccp-pds) — S3 (anonymous access)
- Files are under
data/isccp/(Full) anddata/isccp-basic/hgg|hgh|hgm/(Basic).
- Files are under
- Google Cloud open bucket (noaa-cdr-cloud-properties-isccp) — GCS
- Interim ICDR (2017-07 to 2018-12, FTP) — FTP (
isccp/= Full,isccp_basic/= Basic)- Temporary data, not the official CDR. Chrome and Firefox no longer support FTP, so use an FTP client or command-line tool.
Example code¶
Reads one month of Basic HGM from the AWS open bucket without an account. The file name follows the pattern seen in the bucket listing.
# pip install s3fs xarray h5netcdf
import numpy as np
import s3fs
import xarray as xr
fs = s3fs.S3FileSystem(anon=True)
key = ("noaa-cdr-cloud-properties-isccp-pds/data/isccp-basic/hgm/"
"ISCCP-Basic.HGM.v01r00.GLOBAL.2016.01.99.9999.GPC.10KM.CS00.EA1.00.nc")
ds = xr.open_dataset(fs.open(key), engine="h5netcdf")
ca = ds["cldamt"].squeeze() # monthly mean cloud amount (percent), 1° lat-lon grid
w = np.cos(np.deg2rad(ds["lat"]))
print(float(ca.weighted(w).mean(("lat", "lon")))) # area-weighted global mean
Practical tips¶
- July 2017 onward is not the official CDR. If you extend through 2017–2018, state in your paper that you used the interim ICDR, and use other records after that.
- NCEI's caveats note a two-year gap in polar-orbiter (NOM) data during the NOAA-15 to NOAA-17 transition (2000–2002), and missing visible channels in many MET-3 images in 1995 and GMS-3 images in February–April 1986. Be careful with trends and diurnal analyses in these periods.
- Cloud amount changes by about 0.05 between nadir and slant views. Regional values can step up or down when a geostationary satellite is replaced or relocated.
- Low clouds under thin high cloud are hard to see. The users guide says high cloud is about 0.10 too low and middle cloud about 0.10 too high compared with lidar.
- In the Full version, values are counts. Averaging them without the lookup tables gives numbers with no physical meaning. If you are new to ISCCP, start with the Basic version.
- The Basic version remaps the equal-area grid onto 1° latitude-longitude cells, so at high latitudes several cells share the same original value. Always apply area weighting (cosine of latitude).
Notices and change history¶
2026-09-21 · Info · Follow-on ISCCP-NG demonstrator released (CM SAF, year 2021)
EUMETSAT CM SAF released an ISCCP-NG demonstrator dataset built from global level-1 composites of five geostationary satellites. The first release covers 2021 and provides cloud properties and top-of-atmosphere radiative fluxes at 0.05° and half-hourly resolution. It is a demonstrator, not a long-term record, so it does not yet continue ISCCP-H.
References for your paper¶
Double-check before using in a paper
The citations below were compiled by the maintainer and may contain errors. Always double-check DOIs, authors, years and access-date formats against the provider's official dataset page and your journal's guidelines.
Dataset citation¶
ISCCP H-Series CDR — DOI 10.7289/V5QZ281S
Rossow, W.B., Walker, A., Golea, V., Knapp, K.R., Young, A., Inamdar, A., and Hankins, B., with NOAA's Climate Data Record Program (2016): International Satellite Cloud Climatology Project Climate Data Record, H-Series. NOAA National Centers for Environmental Information. doi:10.7289/V5QZ281S [access date]
Show BibTeX
@misc{isccp_h_cdr,
author = {Rossow, William B. and Walker, Alison and Golea, Violeta and Knapp, Kenneth R. and Young, Alisa and Inamdar, Anand and Hankins, Bill},
title = {International Satellite Cloud Climatology Project Climate Data Record, H-Series},
year = {2016},
publisher = {NOAA National Centers for Environmental Information},
doi = {10.7289/V5QZ281S}
}
Reference papers¶
ISCCP-H product description paper — DOI 10.5194/essd-10-583-2018
Young, A. H., Knapp, K. R., Inamdar, A., Hankins, W., and Rossow, W. B. (2018): The International Satellite Cloud Climatology Project H-Series climate data record product. Earth System Science Data, 10, 583–593.
Show BibTeX
@article{young2018isccph,
author = {Young, Alisa H. and Knapp, Kenneth R. and Inamdar, Anand and Hankins, William and Rossow, William B.},
title = {The International Satellite Cloud Climatology Project {H}-Series climate data record product},
journal = {Earth System Science Data},
volume = {10},
pages = {583--593},
year = {2018},
doi = {10.5194/essd-10-583-2018}
}
Advances in understanding clouds from ISCCP (cited in the NCEI use agreement) — DOI 10.1175/1520-0477(1999)080<2261:AIUCFI>2.0.CO;2
Rossow, W. B., and Schiffer, R. A. (1999): Advances in Understanding Clouds from ISCCP. Bulletin of the American Meteorological Society, 80(11), 2261–2287.
Show BibTeX
@article{rossow1999isccp,
author = {Rossow, William B. and Schiffer, Robert A.},
title = {Advances in Understanding Clouds from {ISCCP}},
journal = {Bulletin of the American Meteorological Society},
volume = {80},
number = {11},
pages = {2261--2287},
year = {1999},
doi = {10.1175/1520-0477(1999)080<2261:AIUCFI>2.0.CO;2}
}
Acknowledgements¶
The NOAA CDR use agreement asks users to state that the data were obtained from NCEI, to credit the CDR developers and their affiliations, and to note NOAA CDR Program support with "Development of the CDR was supported by NOAA's CDR Program." When a CDR is central to the work, it also encourages offering co-authorship to the developers.
If this page helped, please acknowledge the Korean Climate Data Navigator
Please add the sentence below to the Acknowledgements of your paper.