than the C band scatterometer. Monthly flooded areas are calculated by estimating flooded pixel fractional coverage using the altimeter

spatial coverage is achieved in winter due to the comprehensive data coverage by Sentinel-1 and

by a much more capable system with similar time resolutions and global coverage. Get PDF (360 kB

by the City, identify neighborhoods of both adequate and inadequate coverage and provide

used to investigate these feedbacks in high-elevation regions where the coverage of surface

that this radiative flux uncertainty is closely related to the simulated stratiform cloud coverage. Single-moment schemes underestimate

3D Planetary General Circulation Model. We also explain how boundary condition choices such as ocean/lake coverage/depth, rotation rate, atmospheric

seeks to quantify these past rapid responses in temperature and ice coverage on land and

and research. The operational component takes advantage of the global coverage provided by the

in recent years. Several networks operate about a hundred instruments providing good geographical coverage of the

deriving vertically resolved CCN concentrations from lidar observations to expand the spatiotemporal coverage of limited

land and ocean cyclones with similar PW and ω 850 , ice cloud coverage is found to

last more than a few years and it does not provide global coverage. We stress the

measurements in space-time variations across all these scales simultaneously. Satellite constellations with global coverage and high

5 mass that are broadly consistent; however, the adjusted CMAQ values provide greater spatial coverage and information

by Box Behnken Design (BBD), then, all the experiments were modeled by maximized capacitated coverage (MCC) in GIS

accurate and high-resolution aerosol-retrieval products will provide unique spatial and temporal coverage of the

analyze the incoming signal with very different frequency resolutions and total spectral coverage. This has allowed us

of deep tropical convection occurs. Analysis modifications to account for satellite coverage changes during the

thickness, our time series uses velocity maps that begin with sparse spatial and temporal coverage and end

increased considerably in the past decade with spectral, spatial, and temporal coverage. At the same

used to detect inumdation. Monthly flooded aread are then calculated by estimating pixel fractional coverage of flooding

However, in a decidedly nonstatistical approach allowed by the wide-area coverage and the

the same methodology. We find that a large mismatch in geographic coverage exists between the

contribution of those elements to the evolution of ice coverage through spring and

throughout the tropics, then the calculated occurrence frequency and areal coverage of TTL

poor agreement with climate model predictions. These disagreements could be due to insufficient spatial coverage, spatiotemporal biases, or model

about the necessary attributes of a cloud monitoring system. (1) Complete global coverage with uniform density is

the radiative response in high latitudes is sensitive to the coverage of snow

missing values in the dataset which result from the incomplete satellite coverage. Weight coefficients in

resource limitations may prohibit incorporating all best practices into all measurements and that spatial coverage is also an important

combination of resolution and scope in either time or space coverage to properly

a maximum in stratiform rainfall fraction, which was derived independently from radar precipitation coverage area. The ground

complicated by inherent difficulties in measuring E and P with sufficient spatial coverage and resolution

data assimilation (DA) systems are vital. Satellite EOs are particularly relevant, as they offer quasi-global coverage, are non-intrusive, and

increases/decreases with height in the NH/SH. The broader spatial coverage of the

Project (FireMIP) protocol to estimate emissions when the available proxies had limited coverage. According to our

hence O x distributions. Thirdly we reduce sea surface temperatures and increase ocean ice coverage which impact water vapor

quality and local variability. Although more than 1000 locations are documented, the spatial coverage remains uneven with a

satellites operated by weather agencies worldwide. Meeting the ISCCP goals of global coverage and decade

SpectroRadiometer (MODIS) and Multi-angle Imaging Spectroradiomater (MISR) provide regular aerosol observations with global coverage. It is essential to

a spatial resolution of 0.5°. Both surveys had a spectral coverage of 333

S-60°N geographical latitude. We found that, in general, the MODIS coverage causes an underestimate of

validate similar products from other instruments that will have higher spatial resolution and global coverage than APS, but poorer

signal of cirrus contrails over S. E. Asia, we calculated trends in cirrus coverage over tropical regions with

implications of the effect of satellite orbit and spatial coverage, the effect

273, doi:10.1016/j.atmosenv.2014.12.010. Due to their extensive spatial coverage, satellite Aerosol Optical Depth

swath images of several hundred coastal habitats daily. Nine H4 satellites would provide weekly coverage of global

only span parts of the 20th and 21st centuries. Such data coverage is insufficient for