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The search expression was <secondaryty pi and firstg DMD-CPT-INPE-MCTI-GOV-BR and y 2012 and dissemination websci>.
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Search local date and time: 20/04/2024 05:45.

1. Identity statement
Reference Type	Journal Article
Site	plutao.sid.inpe.br
Holder Code	isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier	J8LNKAN8RW/3D53S9L
Repository	dpi.inpe.br/plutao/2012/11.28.17.56.15
Last Update	2013:01.17.15.36.56 (UTC) administrator
Metadata Repository	dpi.inpe.br/plutao/2012/11.28.17.56.16
Metadata Last Update	2021:01.02.03.52.42 (UTC) administrator
Secondary Key	INPE--PRE/
DOI	10.1029/2011WR011347
ISSN	0043-1397
Label	lattes: 6072354470541631 5 YatheendradasLKCGSGCBKTRM:2012:ExOvDM
Citation Key	YatheendradasLKCGSGCBKTRM:2012:ExOvDM
Title	Distributed assimilation of satellite-based snow extent for improving simulated streamflow in mountainous, dense forests: An example over the DMIP2 western basins
Year	2012
Month	Set.
Access Date	2024, Apr. 20
Secondary Type	PRE PI
Number of Files	1
Size	2232 KiB

2. Context
Author	1 Yatheendradas, Soni 2 Lidard, Christa D. Peters 3 Koren, Victor 4 Cosgrove, Brian A. 5 Gonçalves, Luis Gustavo Gonçalves 6 Smith, Michael 7 Geiger, Jim 8 Cui, Zhengtao 9 Borak, Jordan 10 Kumar, Sujay V. 11 Toll, David L. 12 Riggs, George 13 Mizukami, Naoki
Group	1 2 3 4 5 DMD-CPT-INPE-MCTI-GOV-BR
Affiliation	1 Hydrological Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD 20771, United States 2 Hydrological Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD 20771, United States 3 Office of Hydrologic Development, Hydrology Laboratory, National Weather Service, Silver Spring, MD, United States 4 Office of Hydrologic Development, Hydrology Laboratory, National Weather Service, Silver Spring, MD, United States 5 Instituto Nacional de Pesquisas Espaciais (INPE) 6 7 NASA Goddard Space Flight Center, Greenbelt, MD, United States 8 9 10 Science Applications International Corporation, Beltsville, MD, United States 11 Earth System Science Interdisciplinary Center, College Park, MD, United States; Hydrological Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD 20771, United States 12 Science Systems and Applications Inc., Lanham, MD, United States 13 National Center for Atmospheric Research, Boulder, CO, United States
Author e-Mail Address	1 2 3 4 5 gustavo.goncalves@cptec.inpe.br
e-Mail Address	gustavo.goncalves@cptec.inpe.br
Journal	Water Resources Research
Volume	48
Number	9
Pages	W09557
Secondary Mark	A1_CIÊNCIAS_AGRÁRIAS_I A2_ECOLOGIA_E_MEIO_AMBIENTE A1_ENGENHARIAS_I A1_ENGENHARIAS_III A1_INTERDISCIPLINAR A1_PLANEJAMENTO_URBANO_E_REGIONAL_/_DEMOGRAFIA
History (UTC)	2012-11-28 23:06:33 :: lattes -> marciana :: 2012 2013-01-21 11:06:05 :: marciana -> administrator :: 2012 2021-01-02 03:52:42 :: administrator -> marciana :: 2012

3. Content and structure
Is the master or a copy?	is the master
Content Stage	completed
Transferable	1
Content Type	External Contribution
Version Type	publisher
Keywords	REMOTE-SENSING DATA LAND-SURFACE MODEL COVERED AREA WATER EQUIVALENT HYDROLOGIC MODEL SIERRA-NEVADA RIVER-BASIN MODIS VARIABILITY VEGETATION
Abstract	Snow cover area affects snowmelt, soil moisture, evapotranspiration, and ultimately streamflow. For the Distributed Model Intercomparison Project - Phase 2 Western basins, we assimilate satellite-based fractional snow cover area (fSCA) from the Moderate Resolution Imaging Spectroradiometer, or MODIS, into the National Weather Service (NWS) SNOW-17 model. This model is coupled with the NWS Sacramento Heat Transfer (SAC-HT) model inside the National Aeronautics and Space Administration's (NASA) Land Information System. SNOW-17 computes fSCA from snow water equivalent (SWE) values using an areal depletion curve. Using a direct insertion, we assimilate fSCAs in two fully distributed ways: (1) we update the curve by attempting SWE preservation, and (2) we reconstruct SWEs using the curve. The preceding are refinements of an existing simple, conceptually guided NWS algorithm. Satellite fSCA over dense forests inadequately accounts for below-canopy snow, degrading simulated streamflow upon assimilation during snowmelt. Accordingly, we implement a below-canopy allowance during assimilation. This simplistic allowance and direct insertion are found to be inadequate for improving calibrated results, still degrading them as mentioned above. However, for streamflow volume for the uncalibrated runs, we obtain: (1) substantial to major improvements (64-81%) as a percentage of the control run residuals (or distance from observations), and (2) minor improvements (16-22%) as a percentage of observed values. We highlight the need for detailed representations of canopy-snow optical radiative transfer processes in mountainous, dense forest regions if assimilation-based improvements are to be seen in calibrated runs over these areas.
Area	MET
Arrangement	urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Distributed assimilation of...
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4. Conditions of access and use
data URL	http://urlib.net/ibi/J8LNKAN8RW/3D53S9L
zipped data URL	http://urlib.net/zip/J8LNKAN8RW/3D53S9L
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5. Allied materials
Next Higher Units	8JMKD3MGPCW/43SKC35
Dissemination	WEBSCI
Host Collection	dpi.inpe.br/plutao@80/2008/08.19.15.01

6. Notes
Empty Fields	alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup resumeid rightsholder schedulinginformation secondarydate session shorttitle sponsor subject targetfile tertiarymark tertiarytype typeofwork url

7. Description control
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1. Identity statement
Reference Type	Journal Article
Site	plutao.sid.inpe.br
Holder Code	isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier	J8LNKAN8RW/3D53S9H
Repository	dpi.inpe.br/plutao/2012/11.28.17.56.12
Last Update	2013:02.05.18.56.42 (UTC) marciana
Metadata Repository	dpi.inpe.br/plutao/2012/11.28.17.56.13
Metadata Last Update	2021:01.02.03.52.42 (UTC) administrator
DOI	10.5194/hess-16-3127-2012
ISSN	1027-5606
Label	lattes: 6072354470541631 6 PaivaPPCBGCBCGBG:2012:SoHyPr
Citation Key	PaivaCollBonnGonç:2012:SoHyPr
Title	On the sources of hydrological prediction uncertainty in the Amazon
Project	FINEP and ANA (“Projeto de Integração e Cooperação Amazônica para a Modernização do Monitoramento Hidrológico” (ICA-MMH)); CNPq (“Assimilação de Dados de monitoramento Espacial para a análise do regime hidrológico da Bacia Amazônica e a previsão de curto e médio prazos”)
Year	2012
Access Date	2024, Apr. 20
Secondary Type	PRE PI
Number of Files	1
Size	4753 KiB

2. Context
Author	1 Paiva, R. C. D. 2 Collischonn, W. 3 Bonnet, M. P. 4 de Gonçalves, Luis Gustavo Gonçalves
Group	1 2 3 4 DMD-CPT-INPE-MCTI-GOV-BR
Affiliation	1 rodrigocdpaiva@gmail.com 2 3 4 Instituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Address	1 2 3 4 gustavo.goncalves@cptec.inpe.br
e-Mail Address	gustavo.goncalves@cptec.inpe.br
Journal	Hydrology and Earth System Sciences
Volume	16
Number	9
Pages	3127-3137
Secondary Mark	B2_ARQUITETURA_E_URBANISMO B1_CIÊNCIAS_BIOLÓGICAS_I A1_ENGENHARIAS_I A2_GEOGRAFIA
History (UTC)	2012-11-28 23:06:33 :: lattes -> administrator :: 2012 2013-02-05 18:39:09 :: administrator -> marciana :: 2012 2013-02-05 18:56:42 :: marciana -> administrator :: 2012 2021-01-02 03:52:42 :: administrator -> marciana :: 2012

3. Content and structure
Is the master or a copy?	is the master
Content Stage	completed
Transferable	1
Content Type	External Contribution
Version Type	publisher
Keywords	hydrological forecast systems Amazon Ensemble Streamflow Prediction (ESP) reverse Ensemble Streamflow Prediction (reverse-ESP)
Abstract	Recent extreme events in the Amazon River basin and the vulnerability of local population motivate the development of hydrological forecast systems using process based models for this region. In this direction, the knowledge of the source of errors in hydrological forecast systems may guide the choice on improving model structure, model forcings or developing data assimilation systems for estimation of initial model states. We evaluate the relative importance of hydrologic initial conditions and model meteorological forcings errors (precipitation) as sources of stream flow forecast uncertainty in the Amazon River basin. We used a hindcast approach that compares Ensemble Streamflow Prediction (ESP) and a reverse Ensemble Streamflow Prediction (reverse-ESP). Simulations were performed using the physically-based and distributed hydrological model MGB-IPH, comprising surface energy and water balance, soil water, river and floodplain hydrodynamics processes. The model was forced using TRMM 3B42 precipitation estimates. Results show that uncertainty on initial conditions plays an important role for discharge predictability, even for large lead times ( 1 to 3 months) on main Amazonian Rivers. Initial conditions of surface waters state variables are the major source of hydrological forecast uncertainty, mainly in rivers with low slope and large floodplains. Initial conditions of groundwater state variables are important, mostly during low flow period and in the southeast part of the Amazon where lithology and the strong rainfall seasonality with a marked dry season may be the explaining factors. Analyses indicate that hydrological forecasts based on a hydrological model forced with historical meteorological data and optimal initial conditions may be feasible. Also, development of data assimilation methods is encouraged for this region.
Area	MET
Arrangement	urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > On the sources...
doc Directory Content	access
source Directory Content	there are no files
agreement Directory Content	there are no files

4. Conditions of access and use
data URL	http://urlib.net/ibi/J8LNKAN8RW/3D53S9H
zipped data URL	http://urlib.net/zip/J8LNKAN8RW/3D53S9H
Language	en
Target File	hess-16-3127-2012.pdf
User Group	lattes marciana
Visibility	shown
Archiving Policy	allowpublisher allowfinaldraft
Update Permission	not transferred

5. Allied materials
Next Higher Units	8JMKD3MGPCW/43SKC35
Citing Item List	sid.inpe.br/bibdigital/2021/01.01.17.20 1
Dissemination	WEBSCI; PORTALCAPES.
Host Collection	dpi.inpe.br/plutao@80/2008/08.19.15.01

6. Notes
Empty Fields	alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark mirrorrepository month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress readergroup readpermission resumeid rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url

7. Description control
e-Mail (login)	marciana
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1. Identity statement
Reference Type	Journal Article
Site	plutao.sid.inpe.br
Holder Code	isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier	J8LNKAN8RW/3D53ND4
Repository	dpi.inpe.br/plutao/2012/11.28.17.09.11
Last Update	2015:03.13.19.29.15 (UTC) administrator
Metadata Repository	dpi.inpe.br/plutao/2012/11.28.17.09.12
Metadata Last Update	2021:01.02.03.52.41 (UTC) administrator
Secondary Key	INPE--PRE/
DOI	10.1029/2011JD016817
ISSN	0148-0227
Label	lattes: 9873289111461387 5 WebleyStStGrFrPa:2012:AnEy20
Citation Key	WebleyStStGrFrPa:2012:AnEy20
Title	Analyzing the Eyjafjallajökull 2010 eruption using satellite remote sensing, lidar and WRF-Chem dispersion and tracking model
Year	2012
Month	July
Access Date	2024, Apr. 20
Type of Work	journal article
Secondary Type	PRE PI
Number of Files	1
Size	4666 KiB

2. Context
Author	1 Webley, P. W. 2 Steensen, T. 3 Stuefer, Martin 4 Grell, G. 5 Freitas, Saulo Ribeiro de 6 Pavolonis, Michael
Resume Identifier	1 2 3 4 5 8JMKD3MGP5W/3C9JJ7M
Group	1 2 3 4 5 DMD-CPT-INPE-MCTI-GOV-BR
Affiliation	1 University of Alasca 2 University of Alasca 3 University of Alasca 4 5 Instituto Nacional de Pesquisas Espaciais (INPE) 6 National Oceanic and Atmospheric Administration (NOAA)
Author e-Mail Address	1 pwebley@gi.alaska.edu 2 3 4 5 saulo.freitas@cptec.inpe.br
e-Mail Address	saulo.freitas@cptec.inpe.br
Journal	Journal of Geophysical Research
Volume	117
Pages	D00U26
Secondary Mark	B1_ASTRONOMIA_/_FÍSICA B2_CIÊNCIA_DA_COMPUTAÇÃO A1_CIÊNCIAS_AGRÁRIAS_I A1_ECOLOGIA_E_MEIO_AMBIENTE A1_ENGENHARIAS_I A2_ENGENHARIAS_II A1_ENGENHARIAS_III A2_ENGENHARIAS_IV A1_GEOCIÊNCIAS A1_INTERDISCIPLINAR
History (UTC)	2012-11-28 23:06:31 :: lattes -> administrator :: 2012 2012-12-13 17:08:28 :: administrator -> marciana :: 2012 2012-12-13 17:10:47 :: marciana -> administrator :: 2012 2013-01-20 15:55:08 :: administrator -> marciana :: 2012 2013-02-06 16:08:14 :: marciana -> administrator :: 2012 2021-01-02 03:52:41 :: administrator -> marciana :: 2012

3. Content and structure
Is the master or a copy?	is the master
Content Stage	completed
Transferable	1
Content Type	External Contribution
Version Type	publisher
Keywords	ash-cloud transport volcanic ash crater peak source parameters Mount Spurr Alaska plumes AVHRR simulation deposition
Abstract	Volcanic ash forecasting is a critical tool in hazard assessment and operational volcano monitoring. The use of volcanic ash transport and dispersion models allows analysts to determine the future location of ash clouds. In April-May 2010, Eyjafjallajokull in Iceland erupted explosively. Presented here is an evaluation of the volcanic application of the weather research and forecasting in-line chemistry model (WRF-Chem) applied to Eyjafjallajokull. The analysis focuses on the first few days of the explosive events, April 14-19. The model simulations are presented along with multiple satellite and ground based tools to compare and validate the results. The WRF-Chem results showed the ash cloud dispersing toward mainland Europe, with concentrations crossing Europe between 0.5-2.0 mg/m(3), centered at 5 km ASL, +/-1 km. Comparisons with satellite volcanic ash retrievals showed a good agreement and ground-based Light Detection And Ranging (LIDAR) data compared well to the model simulations. The analysis in this manuscript has illustrated the use of WRF-Chem for volcanic eruptions, with the coupled numerical weather simulation and ash forecasting important to understand the local atmospheric conditions as well as the ash cloud distribution. We show that to fully forecast ash concentrations, to the level of mg's per m(3), there is a need for accurate knowledge of the plume height; mass eruption rate; particle size distribution and duration along with a fusion of all data. Then accurate hazard assessments can be performed to limit the impact that dispersing clouds have on the aviation community and population.
Area	MET
Arrangement	urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Analyzing the Eyjafjallajökull...
doc Directory Content	access
source Directory Content	there are no files
agreement Directory Content	there are no files

4. Conditions of access and use
data URL	http://urlib.net/ibi/J8LNKAN8RW/3D53ND4
zipped data URL	http://urlib.net/zip/J8LNKAN8RW/3D53ND4
Language	en
User Group	administrator lattes marciana
Reader Group	administrator marciana
Visibility	shown
Archiving Policy	denypublisher6 allowfinaldraft
Read Permission	allow from all
Update Permission	not transferred

5. Allied materials
Next Higher Units	8JMKD3MGPCW/43SKC35
Dissemination	WEBSCI; AGU; MGA; COMPENDEX.
Host Collection	dpi.inpe.br/plutao@80/2008/08.19.15.01

6. Notes
Empty Fields	alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark mirrorrepository nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate session shorttitle sponsor subject targetfile tertiarymark tertiarytype url

7. Description control
e-Mail (login)	marciana
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1. Identity statement
Reference Type	Journal Article
Site	plutao.sid.inpe.br
Holder Code	isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier	J8LNKAN8RW/3D537SH
Repository	dpi.inpe.br/plutao/2012/11.28.14.13 (restricted access)
Last Update	2013:02.06.12.06.48 (UTC) marciana
Metadata Repository	dpi.inpe.br/plutao/2012/11.28.14.13.30
Metadata Last Update	2021:01.02.03.52.40 (UTC) administrator
Secondary Key	INPE--PRE/
DOI	10.1007/s00704-012-0633-y
ISSN	0177-798X
Label	lattes: 4336175279058172 2 PilottoChanNobr:2012:SeClHi
Citation Key	PilottoChouNobr:2012:SeClHi
Title	Seasonal climate hindcasts with Eta model nested in CPTEC coupled ocean-atmosphere general circulation model
Year	2012
Access Date	2024, Apr. 20
Secondary Type	PRE PI
Number of Files	1
Size	3582 KiB

2. Context
Author	1 Pilotto, Isabel 2 Chou, Sin Chan 3 Nobre, Paulo
Resume Identifier	1 2 3 8JMKD3MGP5W/3C9JJ3B
Group	1 2 DMD-CPT-INPE-MCTI-GOV-BR 3 DMD-CPT-INPE-MCTI-GOV-BR
Affiliation	1 2 Instituto Nacional de Pesquisas Espaciais (INPE) 3 Instituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Address	1 isabel.pilotto@cptec.inpe.br 2 chou@pesquisador.cnpq.br 3 pnobre@cptec.inpe.br
e-Mail Address	chou@pesquisador.cnpq.br
Journal	Theoretical and Applied Climatology
Volume	110
Pages	437-456
Secondary Mark	B2_ASTRONOMIA_/_FÍSICA A2_CIÊNCIAS_AGRÁRIAS_I B1_GEOCIÊNCIAS A2_GEOGRAFIA A2_INTERDISCIPLINAR
History (UTC)	2012-11-28 23:06:21 :: lattes -> administrator :: 2012 2013-01-28 14:02:30 :: administrator -> marciana :: 2012 2013-02-06 12:06:48 :: marciana -> administrator :: 2012 2021-01-02 03:52:40 :: administrator -> marciana :: 2012

3. Content and structure
Is the master or a copy?	is the master
Content Stage	completed
Transferable	1
Content Type	External Contribution
Version Type	publisher
Keywords	regional climate models (RCMs) Eta model CPTEC atmospheric general circulation model South America tropical Atlantic climate hindcasts
Abstract	This work evaluates the added value of the downscaling technique employed with the Eta model nested in the CPTEC atmospheric general circulation model and in the CPTEC coupled oceanatmosphere general circulation model (CGCM). The focus is on the austral summer season, DecemberJanuaryFebruary, with three members each year. Precipitation, latent heat flux, and shortwave radiation flux at the surface hindcast by the models are compared with observational data and model analyses. The global models generally overestimate the precipitation over South America and tropical Atlantic. The CGCM and the nested Eta (Eta + C) both produce a split in the ITCZ precipitation band. The Eta + C produces better precipitation pattern for the studied season. The Eta model reduces the excessive latent heat flux generated by these global models, in particular the Eta + C. Comparison against PIRATA buoys data shows that the Eta + C results in the smallest precipitation and shortwave radiation forecast errors. The Eta + C comparatively best results are though as a consequence of both: the regional model resolution/physics and smaller errors on the lateral boundary conditions provided by the CGCM.
Area	MET
Arrangement	urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Seasonal climate hindcasts...
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4. Conditions of access and use
Language	en
Target File	Pilotto.pdf
User Group	administrator lattes marciana
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Archiving Policy	denypublisher denyfinaldraft12
Read Permission	deny from all and allow from 150.163
Update Permission	not transferred

5. Allied materials
Next Higher Units	8JMKD3MGPCW/43SKC35
URL (untrusted data)	http://link.springer.com/article/10.1007/s00704-012-0633-y?null
Dissemination	WEBSCI; PORTALCAPES; MGA.
Host Collection	dpi.inpe.br/plutao@80/2008/08.19.15.01

6. Notes
Empty Fields	alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark mirrorrepository month nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype typeofwork

7. Description control
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1. Identity statement
Reference Type	Journal Article
Site	plutao.sid.inpe.br
Holder Code	isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier	J8LNKAN8RW/3C647SL
Repository	dpi.inpe.br/plutao/2012/06.21.21.30 (restricted access)
Last Update	2012:08.29.14.16.01 (UTC) administrator
Metadata Repository	dpi.inpe.br/plutao/2012/06.21.21.30.43
Metadata Last Update	2021:01.02.03.52.40 (UTC) administrator
DOI	10.1007/s00703-012-0182-z
ISSN	0177-7971
Label	lattes: 4336175279058172 2 MesingerCGJBBLLMRV:2012:UpVeEt
Citation Key	MesingerCGJBBLLMRV:2012:UpVeEt
Title	An upgraded version of the Eta model
Year	2012
Month	May
Access Date	2024, Apr. 20
Secondary Type	PRE PI
Number of Files	1
Size	1197 KiB

2. Context
Author	1 Mesinger, Fedor 2 Chan, Chou Sin 3 Gomes, Jorge L. 4 Jovic, Dusan 5 Bastos, Paulo 6 Bustamante, Josiane F. 7 Lazic, Lazar 8 Lyra, André A. 9 Morelli, Sandra 10 Ristic, Ivan 11 Veljovic, Katarina
Resume Identifier	1 2 8JMKD3MGP5W/3C9JGRQ
Group	1 2 DMD-CPT-INPE-MCTI-GOV-BR 3 CPT-CPT-INPE-MCTI-GOV-BR 4 5 6 CPT-CPT-INPE-MCTI-GOV-BR 7 8 CPT-CPT-INPE-MCTI-GOV-BR
Affiliation	1 Univ Maryland, ESSIC, College Pk, MD 20742 USA 2 Instituto Nacional de Pesquisas Espaciais (INPE) 3 Instituto Nacional de Pesquisas Espaciais (INPE) 4 NCEP Environm Modeling Ctr, Camp Springs, MD USA 5 Brazilian AF, Brasilia, DF, Brazil 6 Instituto Nacional de Pesquisas Espaciais (INPE) 7 Univ Belgrade, Inst Meteorol, Belgrade, Serbia 8 Instituto Nacional de Pesquisas Espaciais (INPE) 9 Univ Modena & Reggio Emilia, Dept Phys, Modena, Italy 10 Weather2Umbrella Co, Belgrade, Serbia 11 Univ Belgrade, Inst Meteorol, Belgrade, Serbia
Author e-Mail Address	1 fedor@essic.umd.edu 2 chou@pesquisador.cnpq.br
e-Mail Address	chou@pesquisador.cnpq.br
Journal	Meteorology and Atmospheric Physics
Volume	116
Number	3-4
Pages	63-79
Secondary Mark	B1_GEOCIÊNCIAS B1_INTERDISCIPLINAR
History (UTC)	2012-06-22 00:11:01 :: lattes -> administrator :: 2012 2012-07-17 13:05:03 :: administrator -> secretaria.cpa@dir.inpe.br :: 2012 2012-08-29 14:16:01 :: secretaria.cpa@dir.inpe.br -> administrator :: 2012 2021-01-02 03:52:40 :: administrator -> marciana :: 2012

3. Content and structure
Is the master or a copy?	is the master
Content Stage	completed
Transferable	1
Content Type	External Contribution
Version Type	publisher
Keywords	pressure-gradient force volume integration method step-mountain coordinate convective parameterization single-column scheme precipitation atmosphere advection impact
Abstract	Upgrades implemented over a number of years in an open source version of the Eta model, posted at the CPTEC web site http://www.emc.ncep.noaa.gov/mmb/wrkstn_eta, which differs from the NCEP's latest operational Eta by having the WRF-NMM nonhydrostatic option included. Most of the upgrades made resulted from attention paid to less than satisfactory performance noted in several Eta results, and identification of the reasons for the problem. Others came from simple expectation that including a feature that is physically justified but is missing in the code should help. The most notable of the upgrades are the introduction of the so-called sloping steps, or discretized shaved cells topography; piecewise-linear finite-volume vertical advection of dynamic variables; vapor and hydrometeor loading in the hydrostatic equation, and changes aimed at refining the convection schemes available in the Eta. Several other modifications have to do with the calculation of exchange coefficients, conservation in the vertical diffusion, and diagnostic calculation of 10-m winds. Several examples showing improved performance resulting from the dynamics changes are given. One includes a case of unrealistically low temperatures in several mountain basins generated by a centered vertical advection difference scheme's unphysical advection from below ground, removed by its replacement with a finite-volume scheme. Another is that of increased katabatic winds in the Terra Nova Bay Antarctica region. Successful forecast of the severe downslope zonda wind case in the lee of the highest peaks of the Andes is also shown, and some of the recent successful verification results of the use of the upgraded model are pointed out. The code is used at numerous places, and along with setup information it is available for outside users at the CPTEC Eta web site given above.
Area	MET
Arrangement 1	urlib.net > BDMCI > Fonds > Produção anterior à 2021 > CGCPT > An upgraded version...
Arrangement 2	urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > An upgraded version...
doc Directory Content	access
source Directory Content	there are no files
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4. Conditions of access and use
Language	en
Target File	Mesinger_et_al_2012.pdf
User Group	administrator lattes secretaria.cpa@dir.inpe.br
Visibility	shown
Archiving Policy	denypublisher denyfinaldraft12
Read Permission	deny from all and allow from 150.163
Update Permission	not transferred

5. Allied materials
Next Higher Units	8JMKD3MGPCW/3EUPEJL 8JMKD3MGPCW/43SKC35
Dissemination	WEBSCI; PORTALCAPES; COMPENDEX.
Host Collection	dpi.inpe.br/plutao@80/2008/08.19.15.01

6. Notes
Notes	Setores de Atividade: Pesquisa e desenvolvimento científico.
Empty Fields	alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark mirrorrepository nextedition orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url

7. Description control
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1. Identity statement
Reference Type	Journal Article
Site	plutao.sid.inpe.br
Holder Code	isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier	J8LNKAN8RW/3C646BC
Repository	dpi.inpe.br/plutao/2012/06.21.21.10.58
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DOI	10.1029/2011JD016355
ISSN	0148-0227
Label	lattes: 6072354470541631 5 RosolemGupShuZenGon:2012:FuMuIm
Citation Key	RosolemGupShuZenGon:2012:FuMuIm
Title	A fully multiple-criteria implementation of the Sobol method for parameter sensitivity analysis
Project	NASA[NNX09AO33H]; NSF Amazon-PIRE[0730305]; B2-Earthscience; NSF Center for Sustainability of semi-Arid Hydrology and Riparian Areas (SAHRA) under the STC[EAR-9876800]; NSF[DEB-0415977]; US National Science Foundation[AGS-0838491]
Year	2012
Month	Apr.
Access Date	2024, Apr. 20
Type of Work	journal article
Secondary Type	PRE PI
Number of Files	1
Size	750 KiB

2. Context
Author	1 Rosolem, Rafael 2 Gupta, Hoshin V. 3 Shuttleworth, W. James 4 Zeng, Xubin 5 Gonçalves, Luis Gustavo Gonçalves
Group	1 2 3 4 5 DMD-CPT-INPE-MCTI-GOV-BR
Affiliation	1 University of Arizona 2 University of Arizona 3 University of Arizona 4 University of Arizona 5 Instituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Address	1 2 3 4 5 gustavo.goncalves@cptec.inpe.br
e-Mail Address	gustavo.goncalves@cptec.inpe.br
Journal	Journal of Geophysical Research
Volume	117
Pages	D07103
Secondary Mark	B1_ASTRONOMIA_/_FÍSICA B2_CIÊNCIA_DA_COMPUTAÇÃO A1_CIÊNCIAS_AGRÁRIAS_I A1_ECOLOGIA_E_MEIO_AMBIENTE A1_ENGENHARIAS_I A2_ENGENHARIAS_II A1_ENGENHARIAS_III A2_ENGENHARIAS_IV A1_GEOCIÊNCIAS A1_INTERDISCIPLINAR
History (UTC)	2012-06-22 00:11:01 :: lattes -> administrator :: 2012 2012-07-24 13:17:13 :: administrator -> secretaria.cpa@dir.inpe.br :: 2012 2012-07-24 13:22:29 :: secretaria.cpa@dir.inpe.br -> administrator :: 2012 2021-01-02 03:52:40 :: administrator -> marciana :: 2012

3. Content and structure
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Content Stage	completed
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Content Type	External Contribution
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Keywords	hydrologic-models atmospheric gcms carbon-dioxide climate forest amazon exchange fluxes energy sib2
Abstract	We present a novel rank-based fully multiple-criteria implementation of the Sobol' variance-based sensitivity analysis approach that implements an objective strategy to evaluate parameter sensitivity when model evaluation involves several metrics of performance. The method is superior to single-criterion approaches while avoiding the subjectivity observed in "pseudo" multiple-criteria methods. Further, it contributes to our understanding of structural characteristics of a model and simplifies parameter estimation by identifying insensitive parameters that can be fixed to default values during model calibration studies. We illustrate the approach by applying it to the problem of identifying the most influential parameters in the Simple Biosphere 3 (SiB3) model using a network of flux towers in Brazil. We find 27-31 (out of 42) parameters to be influential, most (similar to 78%) of which are primarily associated with physiology, soil, and carbon properties, and that uncertainties in the physiological properties of the model contribute most to total model uncertainty in regard to energy and carbon fluxes. We also find that the second most important model component contributing to the total output uncertainty varies according to the flux analyzed; whereas morphological properties play an important role in sensible heat flux, soil properties are important for latent heat flux, and carbon properties (mainly associated with the soil respiration submodel) are important for carbon flux (as expected). These distinct sensitivities emphasize the need to account for the multioutput nature of land surface models during sensitivity analysis and parameter estimation. Applied to other similar models, our approach can help to establish which soil-plant-atmosphere processes matter most in land surface models of Amazonia and thereby aid in the design of field campaigns to characterize and measure the associated parameters. The approach can also be used with other sensitivity analysis procedures that compute at least two model performance metrics.
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1. Identity statement
Reference Type	Journal Article
Site	plutao.sid.inpe.br
Holder Code	isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier	J8LNKAN8RW/3C643G8
Repository	dpi.inpe.br/plutao/2012/06.21.20.36.42 (restricted access)
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Metadata Repository	dpi.inpe.br/plutao/2012/06.21.20.36.43
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DOI	10.1007/s00704-011-0571-0
ISSN	0177-798X
Label	lattes: 9873289111461387 2 SilvaFreiGiel:2012:RoCoTr
Citation Key	SilvaFreiGiel:2012:RoCoTr
Title	Numerical simulation of the diurnal cycle of rainfall in SW Amazon basin during the 1999 rainy season: the role of convective trigger function
Year	2012
Access Date	2024, Apr. 20
Secondary Type	PRE PI
Number of Files	1
Size	739 KiB

2. Context
Author	1 Silva, Cláudio Moisés Santos e 2 Freitas, Saulo Ribeiro de 3 Gielow, Ralf
Resume Identifier	1 2 8JMKD3MGP5W/3C9JJ7M 3 8JMKD3MGP5W/3C9JJ53
Group	1 2 DMD-CPT-INPE-MCTI-GOV-BR
Affiliation	1 Universidade Federal do Rio Grande do Norte 2 Instituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Address	1 claudio@dfte.ufrn.br 2 saulo.freitas@cptec.inpe.br
e-Mail Address	saulo.freitas@cptec.inpe.br
Journal	Theoretical and Applied Climatology
Volume	109
Pages	473–483
Secondary Mark	B2_ASTRONOMIA_/_FÍSICA A2_CIÊNCIAS_AGRÁRIAS_I B1_GEOCIÊNCIAS A2_GEOGRAFIA A2_INTERDISCIPLINAR
History (UTC)	2012-06-22 00:11:01 :: lattes -> administrator :: 2012 2012-07-25 08:17:16 :: administrator -> secretaria.cpa@dir.inpe.br :: 2012 2012-08-29 16:55:18 :: secretaria.cpa@dir.inpe.br -> administrator :: 2012 2021-01-02 03:52:39 :: administrator -> marciana :: 2012

3. Content and structure
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Content Stage	completed
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Abstract	In continental areas, the maximum rainfall simulated with the Brazilian developments on the Regional Atmospheric Modeling System (BRAMS) occurs around 4 h earlier than the one observed with rain gauges. This work presents the successful implementation of a new convective trigger function (CTF) in the convective parameterization scheme used in BRAMS that corrects this misfit between model and observations. The importance of the CTF formulation on the diurnal cycle of rainfall over the Amazon Basin is reflected by the following numbers: Over Rondonia (SWAmazonia), the original version of BRAMS simulates the maximum rainfall at 1400 UTC (1000 LST), with the new CTF maximum shifting to 1800 UTC (1400 LST), while the S-band radar rainfall maximum is at 1900 UTC (1500 LST). This is attributed to two factors: (1) the new CTF is now coupled to the sensible and latent heat fluxes at surface; (2) during the early morning, the convective available potential energy is reduced.
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Arrangement	urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Numerical simulation of...
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Host Collection	dpi.inpe.br/plutao@80/2008/08.19.15.01

6. Notes
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1. Identity statement
Reference Type	Journal Article
Site	plutao.sid.inpe.br
Holder Code	isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier	J8LNKAN8RW/3C643EL
Repository	dpi.inpe.br/plutao/2012/06.21.20.36
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Metadata Repository	dpi.inpe.br/plutao/2012/06.21.20.36.40
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DOI	10.1029/2011MS000084
ISSN	1942-2466
Label	lattes: 9873289111461387 1 FreitasRodrLongPane:2012:ImMoAd
Citation Key	FreitasRodrLongPane:2012:ImMoAd
Title	Impact of a monotonic advection scheme with low numerical diffusion on transport modeling of emissions from biomass burning
Project	CNPq 302696/2008-3, 309922/2007-0
Year	2012
Access Date	2024, Apr. 20
Secondary Type	PRE PI
Number of Files	1
Size	11644 KiB

2. Context
Author	1 Freitas, Saulo Ribeiro de 2 Rodrigues, Lucia F. 3 Longo, Karla Maria 4 Panetta, Jairo
Resume Identifier	1 8JMKD3MGP5W/3C9JJ7M 2 3 8JMKD3MGP5W/3C9JHKQ
Group	1 DMD-CPT-INPE-MCTI-GOV-BR 2 CPT-CPT-INPE-MCTI-GOV-BR 3 DGE-CEA-INPE-MCTI-GOV-BR 4 CPT-CPT-INPE-MCTI-GOV-BR
Affiliation	1 Instituto Nacional de Pesquisas Espaciais (INPE) 2 Instituto Nacional de Pesquisas Espaciais (INPE) 3 Instituto Nacional de Pesquisas Espaciais (INPE) 4 Instituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Address	1 saulo.freitas@cptec.inpe.br
e-Mail Address	saulo.freitas@cptec.inpe.br
Journal	Journal of Advances in Modeling Earth Systems
Volume	3
Number	M01001
Pages	26pp
History (UTC)	2012-06-22 00:11:01 :: lattes -> secretaria.cpa@dir.inpe.br :: 2012 2012-08-29 13:38:42 :: secretaria.cpa@dir.inpe.br -> administrator :: 2012 2012-10-01 13:08:30 :: administrator -> secretaria.cpa@dir.inpe.br :: 2012 2012-10-16 16:49:12 :: secretaria.cpa@dir.inpe.br -> administrator :: 2012 2021-01-02 03:52:39 :: administrator -> marciana :: 2012

3. Content and structure
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Content Stage	completed
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Keywords	System catt-brams brazilian developments atmospheric transport chemistry models coupled aerosol plume rise conservation sensitivity algorithms
Abstract	An advection scheme, which maintains the initial monotonic characteristics of a tracer field being transported and at the same time produces low numerical diffusion, is implemented in the Coupled Chemistry-Aerosol-Tracer Transport model to the Brazilian developments on the Regional Atmospheric Modeling System (CCATT-BRAMS). Several comparisons of transport modeling using the new and original (non-monotonic) CCATT-BRAMS formulations are performed. Idealized 2-D non-divergent or divergent and stationary or time-dependent wind fields are used to transport sharply localized tracer distributions, as well as to verify if an existent correlation of the mass mixing ratios of two interrelated tracers is kept during the transport simulation. Further comparisons are performed using realistic 3-D wind fields. We then perform full simulations of real cases using data assimilation and complete atmospheric physics. In these simulations, we address the impacts of both advection schemes on the transport of biomass burning emissions and the formation of secondary species from non-linear chemical reactions of precursors. The results show that the new scheme produces much more realistic transport patterns, without generating spurious oscillations and under- and overshoots or spreading mass away from the local peaks. Increasing the numerical diffusion in the original scheme in order to remove the spurious oscillations and maintain the monotonicity of the transported field causes excessive smoothing in the tracer distribution, reducing the local gradients and maximum values and unrealistically spreading mass away from the local peaks. As a result, huge differences (hundreds of %) for relatively inert tracers (like carbon monoxide) are found in the smoke plume cores. In terms of the secondary chemical species formed by non-linear reactions (like ozone), we found differences of up to 50% in our simulations.
Area	MET
Arrangement 1	urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDGE > Impact of a...
Arrangement 2	urlib.net > CGCPT > Impact of a...
Arrangement 3	urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Impact of a...
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Next Higher Units	8JMKD3MGPCW/3EU29DP 8JMKD3MGPCW/3EUPEJL 8JMKD3MGPCW/43SKC35
Citing Item List	sid.inpe.br/bibdigital/2013/10.06.18.03 2 sid.inpe.br/mtc-m21/2012/07.13.14.53.10 1
URL (untrusted data)	http://www.agu.org/journals/ms/ms1201/2011MS000084/
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Host Collection	dpi.inpe.br/plutao@80/2008/08.19.15.01

6. Notes
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1. Identity statement
Reference Type	Journal Article
Site	plutao.sid.inpe.br
Holder Code	isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier	J8LNKAN8RW/3C63EN8
Repository	dpi.inpe.br/plutao/2012/06.21.17.25 (restricted access)
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Metadata Last Update	2021:01.02.03.52.38 (UTC) administrator
DOI	10.1007/s00704-011-0560-3
ISSN	0177-798X
Label	lattes: 5465249419038855 1 FranchitoRaoFern:2012:ImGlWa
Citation Key	FranchitoRaoFern:2012:ImGlWa
Title	Tropical land savannization: impact of global warming
Year	2012
Access Date	2024, Apr. 20
Secondary Type	PRE PI
Number of Files	1
Size	283 KiB

2. Context
Author	1 Franchito, Sergio Henrique 2 Rao, V. B. 3 Fernandez, J. P. R.
Resume Identifier	1 8JMKD3MGP5W/3C9JJ82
Group	1 DMD-CPT-INPE-MCTI-GOV-BR 2 3 DMD-CPT-INPE-MCTI-GOV-BR
Affiliation	1 Instituto Nacional de Pesquisas Espaciais (INPE) 2 3 Instituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Address	1 sergio.franchito@cptec.inpe.br
e-Mail Address	fran@cptec.inpe.br
Journal	Theoretical and Applied Climatology
Volume	109
Pages	73-79
Secondary Mark	B2_ASTRONOMIA_/_FÍSICA A2_CIÊNCIAS_AGRÁRIAS_I B1_GEOCIÊNCIAS A2_GEOGRAFIA A2_INTERDISCIPLINAR
History (UTC)	2012-06-22 00:10:59 :: lattes -> administrator :: 2012 2012-07-25 07:37:57 :: administrator -> secretaria.cpa@dir.inpe.br :: 2012 2012-08-29 13:13:17 :: secretaria.cpa@dir.inpe.br -> administrator :: 2012 2013-01-20 15:52:47 :: administrator -> secretaria.cpa@dir.inpe.br :: 2012 2013-01-28 13:36:08 :: secretaria.cpa@dir.inpe.br -> administrator :: 2012 2021-01-02 03:52:38 :: administrator -> marciana :: 2012

3. Content and structure
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Keywords	global warming tropical land regions greenhouse gas
Abstract	This study investigates the impact of global warming on the savannization of the tropical land region and also examines the relative roles of the impact of the increase of greenhouse gas concentration and future changes in land cover on the tropical climate. For this purpose, a mechanisticstatisticaldynamical climate model with a bidirectional interaction between vegetation and climate is used. The results showed that climate change due to deforestation is more than that due to greenhouse gases in the tropical region. The warming due to deforestation corresponds to around 60% of the warming in the tropical region when the increase of CO2 concentration is included together. However, the global warming due to deforestation is negligible. On the other hand, with the increase of CO2 concentration projected for 2100, there is a lower decrease of evapotranspiration, precipitation and net surface radiation in the tropical region compared with the case with only deforestation. Differently from the case with only deforestation, the effect of the changes in the net surface radiation overcomes that due to the evapotranspiration, so that the warming in the tropical land region is increased. The impact of the increase of CO2 concentration on a deforestation scenario is to increase the reduction of the areas covered by tropical forest (and a corresponding increase in the areas covered by savanna) which may reach 7.5% in future compared with the present climate. Compared with the case with only deforestation, drying may increase by 66.7%. This corroborates with the hypothesis that the process of savannization of the tropical forest can be accelerated in future due to global warming.
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Arrangement	urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Tropical land savannization:...
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6. Notes
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1. Identity statement

Reference Type

Journal Article

Site

mtc-m16d.sid.inpe.br

Holder Code

isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S

Identifier

8JMKD3MGP7W/3CF9KF5

Repository

sid.inpe.br/mtc-m19/2012/08.17.11.47

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Metadata Repository

sid.inpe.br/mtc-m19/2012/08.17.11.47.05

Metadata Last Update

2021:01.02.03.52.19 (UTC) administrator

Secondary Key

INPE--PRE/

DOI

10.1175/JCLI-D-11-00444.1

ISSN

0894-8755

Citation Key

NobreAlmeMalaGiar:2012:CoOcVa

Title

Coupled ocean-atmosphere variations over the south atlantic ocean

Project

FAPESP (2005/00915-2)

Year

2012

Month

Set.

Access Date

2024, Apr. 20

Secondary Type

PRE PI

Number of Files

Size

2153 KiB

2. Context

Author

1 Nobre, Paulo
2 Almeida, Roberto A. De
3 Malagutti, Marta
4 Giarolla, Emanuel

Resume Identifier

1 8JMKD3MGP5W/3C9JJ3B
2
3
4 8JMKD3MGP5W/3C9JH2A

Group

1 DMD-CPT-INPE-MCTI-GOV-BR
2 CST-CST-INPE-MCTI-GOV-BR
3 DMD-CPT-INPE-MCTI-GOV-BR
4 DMD-CPT-INPE-MCTI-GOV-BR

Affiliation

1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Instituto Nacional de Pesquisas Espaciais (INPE)

Author e-Mail Address

1 paulo.nobre@cptec.inpe.br
2 roberto.de.almeida@cptec.inpe.br
3
4 emanuel@cptec.inpe.br

Journal

Journal of Climate

Volume

Number

Pages

6349 6358

Secondary Mark

A1_CIÊNCIAS_AGRÁRIAS_I A1_CIÊNCIAS_BIOLÓGICAS_I A1_ECOLOGIA_E_MEIO_AMBIENTE A1_ENGENHARIAS_I A1_GEOCIÊNCIAS A1_INTERDISCIPLINAR

History (UTC)

2012-08-17 11:50:47 :: marciana -> administrator :: 2012
2012-11-21 14:55:51 :: administrator -> marciana :: 2012
2013-01-18 14:26:20 :: marciana -> administrator :: 2012
2013-01-20 15:47:33 :: administrator -> marciana :: 2012
2013-02-07 16:53:53 :: marciana -> administrator :: 2012
2021-01-02 03:52:19 :: administrator -> marciana :: 2012

3. Content and structure

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is the master

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completed

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Abstract

The role of ocean-atmosphere interactions on summer rainfall over the South Atlantic Ocean is explored through the use of coupled ocean-atmosphere models. The Brazilian Center for Weather Forecast and Climate Studies (CPTEC) coupled ocean-atmosphere general circulation model (CGCM) and its atmospheric general circulation model (AGCM) are used to gauge the role of coupled modes of variability of the climate system over the South Atlantic on seasonal timescales. Twenty six years of summer (DJF) simulations were done in ensemble mode with the CGCM, and the AGCM forced with both observed sea surface temperature (SST) and the SST generated by the CGCM forecasts to investigate the dynamics/thermodynamics of the two major convergence zones in the Tropical Atlantic; the Intertropical Convergence Zone (ITCZ) and the South Atlantic Convergence Zone (SACZ). The results present both numerical model and observational evidence supporting the hypothesis that the ITCZ is a thermally direct, SST driven atmospheric circulation, while the SACZ is a thermally indirect atmospheric circulation controlling SST variability underneath-a consequence of ocean-atmosphere interactions not captured by the atmospheric model forced by prescribed ocean temperatures. Six CGCM model results of the ENSEMBLES project, NCEP/NCAR reanalysis data, and ocean and atmospheric data from buoys of the Prediction and Research Moored Array in the Tropical Atlantic (PIRATA) Project over the tropical Atlantic are used to validate the CPTECs coupled and uncoupled models simulations.

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MET

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8JMKD3MGPCW/3F3T29H
8JMKD3MGPCW/43SKC35

Citing Item List

sid.inpe.br/mtc-m21/2012/07.13.14.57.54 1

Dissemination

WEBSCI; PORTALCAPES; AGU; MGA; COMPENDEX.

Host Collection

sid.inpe.br/mtc-m19@80/2009/08.21.17.02

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