The combination of the sea air, the sunshine and the balmy weather and clear blue skies are what wedding dreams are made of and the locations surrounding Port Douglas are just the icing on the cake.
Not exact matches
What this course lacks in
sea views, as offered by most
of the ocean - facing and cliff - top golf courses along Bali's coastal resort areas, Handara Golf makes up for with its great
combination of flowing bentgrass greens backed by lush shrubbery, tropical gardens and mountain panoramas, together with the cool mountain
air that allows for pleasant rounds
of golfing throughout the 18 - hole golf course.
The popularity
of the resort is due to the perfect
combination of the
sea with sandy beaches, mineral springs and mountain clear
air.
The popularity
of the resort is due to the unique
combination of sandy beaches, mountain crystal clear
air, mineral springs and the
sea.
Guests at all three Bay Gardens properties have access to a wide selection
of thrilling land,
sea,
air, and
combination tours that explore the essence
of St. Lucia, its culture, and beauty.
Canadian Ice Service, 4.7, Multiple Methods As with CIS contributions in June 2009, 2010, and 2011, the 2012 forecast was derived using a
combination of three methods: 1) a qualitative heuristic method based on observed end -
of - winter arctic ice thicknesses and extents, as well as an examination
of Surface
Air Temperature (SAT),
Sea Level Pressure (SLP) and vector wind anomaly patterns and trends; 2) an experimental Optimal Filtering Based (OFB) Model, which uses an optimal linear data filter to extrapolate NSIDC's September Arctic Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
Sea Level Pressure (SLP) and vector wind anomaly patterns and trends; 2) an experimental Optimal Filtering Based (OFB) Model, which uses an optimal linear data filter to extrapolate NSIDC's September Arctic Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and
sea ice predicto
sea ice predictors.
Canadian Ice Service, 4.7 (+ / - 0.2), Heuristic / Statistical (same as June) The 2015 forecast was derived by considering a
combination of methods: 1) a qualitative heuristic method based on observed end -
of - winter Arctic ice thickness extents, as well as winter Surface
Air Temperature,
Sea Level Pressure and vector wind anomaly patterns and trends; 2) a simple statistical method, Optimal Filtering Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
Sea Level Pressure and vector wind anomaly patterns and trends; 2) a simple statistical method, Optimal Filtering Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September
sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and
sea ice predicto
sea ice predictors.
Shorefast ice conditions along the northeastern Chukchi
Sea coast (Barrow to Wainwright) reflect the
combination of late freeze - up after the 2012 record minimum summer ice extent and persistent westerly flow advecting warm
air throughout fall and early winter.
The rains, at least meteorologically speaking, were not unexpected; the
combination of slow - moving, low - pressure tropical
air mass fed by high
sea surface temperatures, and record humidity — in addition to the unpredictability
of climate change — make catastrophic floods more likely.
[13] According to Arctic researcher Jennifer Francis, «The Arctic warmth is the result
of a
combination of record - low
sea - ice extent for this time
of year, probably very thin ice, and plenty
of warm / moist
air from lower latitudes being driven northward by a very wavy jet stream.»
Canadian Ice Service; 5.0; Statistical As with Canadian Ice Service (CIS) contributions in June 2009 and June 2010, the 2011 forecast was derived using a
combination of three methods: 1) a qualitative heuristic method based on observed end -
of - winter Arctic Multi-Year Ice (MYI) extents, as well as an examination
of Surface
Air Temperature (SAT),
Sea Level Pressure (SLP) and vector wind anomaly patterns and trends; 2) an experimental Optimal Filtering Based (OFB) Model which uses an optimal linear data filter to extrapolate NSIDC's September Arctic Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere, and sea ice predicto
Sea Level Pressure (SLP) and vector wind anomaly patterns and trends; 2) an experimental Optimal Filtering Based (OFB) Model which uses an optimal linear data filter to extrapolate NSIDC's September Arctic Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere, and
sea ice predicto
sea ice predictors.
Canadian Ice Service, 4.7 (± 0.2), Heuristic / Statistical (same as June) The 2015 forecast was derived by considering a
combination of methods: 1) a qualitative heuristic method based on observed end -
of - winter Arctic ice thickness extents, as well as winter Surface
Air Temperature,
Sea Level Pressure and vector wind anomaly patterns and trends; 2) a simple statistical method, Optimal Filtering Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
Sea Level Pressure and vector wind anomaly patterns and trends; 2) a simple statistical method, Optimal Filtering Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September
sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and
sea ice predicto
sea ice predictors.
I mistakenly believed the increase in ice formation resulted from some
combination of colder
sea water and
air.
The new satellite Qa10 are used in
combination with the newly reprocessed QuikSCAT V3, the latest version
of sea surface temperature (SST) analyses, and with 10m
air temperature estimated from the European Centre for Medium Weather Forecasts (ECMWF) re-analyses (ERA Interim).
As with previous CIS contributions, the 2016 forecast was derived by considering a
combination of methods: 1) a qualitative heuristic method based on observed end -
of - winter Arctic ice thickness / extent, as well as winter surface
air temperature, spring ice conditions and the summer temperature forecast; 2) a simple statistical method, Optimal Filtering Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September
sea ice extent time - series into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and
sea ice predictors.
The
air can be warmer than the
sea surface in some cases due to a
combination of evaporation and radiation from the
sea surface through the optical window direct to space on a clear night, removing energy faster than the
air could add energy by conduction, or if winds bring in hotter
air than the surface film from a different location.
Because Arctic
sea ice is influenced by both
air and water temperatures, the study authors use a
combination of Arctic ice core, tree - ring and lake sediments to reconstruct Arctic conditions over the last 2,000 years.
«Fs», the fixed SST forcing, is a
combination of the flux change at the top
of (and throughout) the atmosphere and
of the global surface
air temperature change after the forcing and with observed
sea surface temperature (SST) and
sea ice (SI) held fixed.