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Maximum Lake sentence examples within 2 Maximum Lake

2 Maximum Lake

Besides, George VI Ice Shelf is analyzed for intra-annual lake dynamics throughout austral summer 2019/2020 and decision-level fused Sentinel-1 and Sentinel-2 maximum lake extent mapping products are presented for selected time periods.

A novel technique for automated mapping of Antarctic supraglacial lakes in Sentinel-1 SAR imagery using deep learning

2 Maximum Lake

In addition, George VI Ice Shelf is analyzed for intra-annual lake dynamics throughout austral summer 2019/2020 and a decision-level fused Sentinel-1 and Sentinel-2 maximum lake extent mapping product is presented for January 2020 revealing a more complete supraglacial lake coverage (~770 km2) than the individual single-sensor products.

A Novel Method for Automated Supraglacial Lake Mapping in Antarctica Using Sentinel-1 SAR Imagery and Deep Learning

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Maximum Lake sentence examples within maximum lake depth

maximum lake depth

Maximum lake depth and the proportion of lake area under the top of the metalimnion were the most important variables to predict the likelihood of hypolimnetic anoxia, which correctly predicted anoxic condition in 84% of lakes (Model 1).

Predicting anoxia in low-nutrient temperate lakes.

maximum lake depth

Results Water temperature degree days and maximum lake depth were two leading predictors influencing both invasion risk and abundance, but they were relatively less important for predicting abundance than other water quality measures.

Species distribution models for invasive Eurasian watermilfoil highlight the importance of data quality and limitations of discrimination accuracy metrics

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Maximum Lake sentence examples within maximum lake level

maximum lake level

Our results show that in 2016 lake level was the lowest of the past 44 years whereas the maximum lake level was recorded in 1985 (+11.

Quantifying recent lake level changes in Patagonia (Argentina and Chile): Back to the future?

maximum lake level

Annual series of peak discharge or maximum lake level, in agreement with previous studies, display increased frequency of floods in the mid-19th century and decreased frequency after the Second World War.

Causes of increased flood frequency in central Europe in the 19th century

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Maximum Lake sentence examples within maximum lake surface

maximum lake surface

Annual maximum lake surface temperature influences ecosystem structure and function and, in particular, the rates of metabolic activities, species survival and biogeography.

Increasing maximum lake surface temperature under climate change

maximum lake surface

We carried out a quantitative analysis of and provided a discussion on the changes in the maximum lake surface water temperature (MLSWT) from 2001 to 2018 at two timescales (month and year) based on MODIS 11A2 composite product data and water temperature environment of cyanobacteria outbreaks.

Maximum lake surface water temperatures changing characteristics under climate change

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Maximum Lake sentence examples within maximum lake evaporation

maximum lake evaporation

There was a ∼  5-month lag between the maximum net radiation (June) and maximum lake evaporation (November).

Contrasting hydrological and thermal intensities determine seasonal lake-level variations – a case study at Paiku Co on the southern Tibetan Plateau

maximum lake evaporation

There was ~5 month lag between the maximum lake evaporation and maximum net radiation at Paiku Co.

Thermal regime, energy budget and lake evaporation at Paiku Co, a deep alpine lake in the central Himalayas

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Maximum Lake sentence examples within maximum lake extent

maximum lake extent

Besides, George VI Ice Shelf is analyzed for intra-annual lake dynamics throughout austral summer 2019/2020 and decision-level fused Sentinel-1 and Sentinel-2 maximum lake extent mapping products are presented for selected time periods.

A novel technique for automated mapping of Antarctic supraglacial lakes in Sentinel-1 SAR imagery using deep learning

maximum lake extent

In addition, George VI Ice Shelf is analyzed for intra-annual lake dynamics throughout austral summer 2019/2020 and a decision-level fused Sentinel-1 and Sentinel-2 maximum lake extent mapping product is presented for January 2020 revealing a more complete supraglacial lake coverage (~770 km2) than the individual single-sensor products.

A Novel Method for Automated Supraglacial Lake Mapping in Antarctica Using Sentinel-1 SAR Imagery and Deep Learning

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10.1007/s10584-021-03085-1

Annual maximum lake surface temperature influences ecosystem structure and function and, in particular, the rates of metabolic activities, species survival and biogeography.

Increasing maximum lake surface temperature under climate change

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10.1002/eap.2361

Maximum lake depth and the proportion of lake area under the top of the metalimnion were the most important variables to predict the likelihood of hypolimnetic anoxia, which correctly predicted anoxic condition in 84% of lakes (Model 1).

Predicting anoxia in low-nutrient temperate lakes.

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10.1007/s12145-021-00714-2

The maximum lake area appeared in March 2015 with 3550.

Geospatial quantitative analysis of the Aral Sea Shoreline changes using RS and GIS techniques

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10.1002/ece3.8002

Results Water temperature degree days and maximum lake depth were two leading predictors influencing both invasion risk and abundance, but they were relatively less important for predicting abundance than other water quality measures.

Species distribution models for invasive Eurasian watermilfoil highlight the importance of data quality and limitations of discrimination accuracy metrics

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10.1371/journal.pone.0254793

At the time of sampling in September 2017, the maximum lake depth was ~1 m.

Rapa Nui (Easter Island) Rano Raraku crater lake basin: Geochemical characterization and implications for the Ahu-Moai Period

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10.1016/J.CATENA.2021.105589

However, bathymetric surveys conducted in October 2015 and September 2019 indicated that the maximum lake depth increased by 0.

Potential catastrophic water outflow from Lake Dian, China: Possible hydrological and ecological risks

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10.5194/EGUSPHERE-EGU21-8467

Our results show that in 2016 lake level was the lowest of the past 44 years whereas the maximum lake level was recorded in 1985 (+11.

Quantifying recent lake level changes in Patagonia (Argentina and Chile): Back to the future?

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10.1002/JQS.3348

Our study pushes back the timing of maximum lake depth at Lake George to at least MIS 3, rather than MIS 2.

Revisiting the abandoned shorelines of Lake George, Australia: a refined optical dating framework

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10.1007/s10347-020-00611-y

The lacustrine carbonates are associated with maximum lake expansions, and are laterally interfingering with fan deltas, as indicated by abundant clastic grains in the intercalations of the skeletal stromatolites.

Lower Triassic (Induan) stromatolites and oolites of the Bernburg Formation revisited – microfacies and palaeoenvironment of lacustrine carbonates in Central Germany

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10.1007/s11356-021-15621-8

We carried out a quantitative analysis of and provided a discussion on the changes in the maximum lake surface water temperature (MLSWT) from 2001 to 2018 at two timescales (month and year) based on MODIS 11A2 composite product data and water temperature environment of cyanobacteria outbreaks.

Maximum lake surface water temperatures changing characteristics under climate change

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10.5194/egusphere-egu21-508

Besides, George VI Ice Shelf is analyzed for intra-annual lake dynamics throughout austral summer 2019/2020 and decision-level fused Sentinel-1 and Sentinel-2 maximum lake extent mapping products are presented for selected time periods.

A novel technique for automated mapping of Antarctic supraglacial lakes in Sentinel-1 SAR imagery using deep learning

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10.3390/rs13020197

In addition, George VI Ice Shelf is analyzed for intra-annual lake dynamics throughout austral summer 2019/2020 and a decision-level fused Sentinel-1 and Sentinel-2 maximum lake extent mapping product is presented for January 2020 revealing a more complete supraglacial lake coverage (~770 km2) than the individual single-sensor products.

A Novel Method for Automated Supraglacial Lake Mapping in Antarctica Using Sentinel-1 SAR Imagery and Deep Learning

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10.5194/HESS-25-3163-2021

There was a ∼  5-month lag between the maximum net radiation (June) and maximum lake evaporation (November).

Contrasting hydrological and thermal intensities determine seasonal lake-level variations – a case study at Paiku Co on the southern Tibetan Plateau

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10.5194/EGUSPHERE-EGU21-15050

In contrast to these simulation studies, we investigate the<strong> </strong>range of simulated West African monsoon precipitation changes caused by a small and a potential maximum lake and wetland extent during the mid-Holocene.

Influence of a small and maximum lake and wetland extent on the simulated West African monsoon precipitation during the mid-Holocene

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10.5194/hess-2019-421

There was ~5 month lag between the maximum lake evaporation and maximum net radiation at Paiku Co.

Thermal regime, energy budget and lake evaporation at Paiku Co, a deep alpine lake in the central Himalayas

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10.1101/572925

We found evidence that thermal preferences influence how species9 depth use and biomass changed with lake size, proportion of littoral area, and maximum lake depth, although we found no relationship with lake shape.

Thermal preference influences depth use but not biomass of predatory fishes in response to lake morphometry

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10.5194/CP-15-1395-2019

Annual series of peak discharge or maximum lake level, in agreement with previous studies, display increased frequency of floods in the mid-19th century and decreased frequency after the Second World War.

Causes of increased flood frequency in central Europe in the 19th century

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10.1080/01431161.2018.1519281

The focus is on April, the stage of maximum lake ice thickness, for the years 2016 and 2017.

The role of lake size and local phenomena for monitoring ground-fast lake ice

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10.1016/J.PALAEO.2019.03.018

The Inle Lake record compares with Holocene sequences in China, Thailand and India and marine cores south of Myanmar, which similarly show a regional pattern of drier conditions in the early Greenlandian stage, followed by maximum lake levels in the early Northgrippian stage.

Holocene environmental change at Inle Lake, Shan State, Myanmar, and its implications for the regional development of agriculture

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10.1111/FME.12327

Maximum lake depth and the presence of mixed fish communities (i.

Potential climate change impacts on Arctic char Salvelinus alpinus L. in Ireland

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10.1016/J.CATENA.2019.02.020

The maximum lake surface area was 965.

Dynamic detection of water surface area of Ebinur Lake using multi-source satellite data (Landsat and Sentinel-1A) and its responses to changing environment

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What is/are Maximum Lake?

Maximum Lake - Annual maximum lake surface temperature influences ecosystem structure and function and, in particular, the rates of metabolic activities, species survival and biogeography. [1] Maximum lake depth and the proportion of lake area under the top of the metalimnion were the most important variables to predict the likelihood of hypolimnetic anoxia, which correctly predicted anoxic condition in 84% of lakes (Model 1). [2] The maximum lake area appeared in March 2015 with 3550. [3] Results Water temperature degree days and maximum lake depth were two leading predictors influencing both invasion risk and abundance, but they were relatively less important for predicting abundance than other water quality measures. [4] At the time of sampling in September 2017, the maximum lake depth was ~1 m. [5] However, bathymetric surveys conducted in October 2015 and September 2019 indicated that the maximum lake depth increased by 0. [6] Our results show that in 2016 lake level was the lowest of the past 44 years whereas the maximum lake level was recorded in 1985 (+11. [7] Our study pushes back the timing of maximum lake depth at Lake George to at least MIS 3, rather than MIS 2. [8] The lacustrine carbonates are associated with maximum lake expansions, and are laterally interfingering with fan deltas, as indicated by abundant clastic grains in the intercalations of the skeletal stromatolites. [9] We carried out a quantitative analysis of and provided a discussion on the changes in the maximum lake surface water temperature (MLSWT) from 2001 to 2018 at two timescales (month and year) based on MODIS 11A2 composite product data and water temperature environment of cyanobacteria outbreaks. [10] Besides, George VI Ice Shelf is analyzed for intra-annual lake dynamics throughout austral summer 2019/2020 and decision-level fused Sentinel-1 and Sentinel-2 maximum lake extent mapping products are presented for selected time periods. [11] In addition, George VI Ice Shelf is analyzed for intra-annual lake dynamics throughout austral summer 2019/2020 and a decision-level fused Sentinel-1 and Sentinel-2 maximum lake extent mapping product is presented for January 2020 revealing a more complete supraglacial lake coverage (~770 km2) than the individual single-sensor products. [12] There was a ∼  5-month lag between the maximum net radiation (June) and maximum lake evaporation (November). [13] In contrast to these simulation studies, we investigate the range of simulated West African monsoon precipitation changes caused by a small and a potential maximum lake and wetland extent during the mid-Holocene. [14] There was ~5 month lag between the maximum lake evaporation and maximum net radiation at Paiku Co. [15] We found evidence that thermal preferences influence how species9 depth use and biomass changed with lake size, proportion of littoral area, and maximum lake depth, although we found no relationship with lake shape. [16] Annual series of peak discharge or maximum lake level, in agreement with previous studies, display increased frequency of floods in the mid-19th century and decreased frequency after the Second World War. [17] The focus is on April, the stage of maximum lake ice thickness, for the years 2016 and 2017. [18] The Inle Lake record compares with Holocene sequences in China, Thailand and India and marine cores south of Myanmar, which similarly show a regional pattern of drier conditions in the early Greenlandian stage, followed by maximum lake levels in the early Northgrippian stage. [19] Maximum lake depth and the presence of mixed fish communities (i. [20] The maximum lake surface area was 965. [21]

2 Maximum Lake

Besides, George VI Ice Shelf is analyzed for intra-annual lake dynamics throughout austral summer 2019/2020 and decision-level fused Sentinel-1 and Sentinel-2 maximum lake extent mapping products are presented for selected time periods. [1] In addition, George VI Ice Shelf is analyzed for intra-annual lake dynamics throughout austral summer 2019/2020 and a decision-level fused Sentinel-1 and Sentinel-2 maximum lake extent mapping product is presented for January 2020 revealing a more complete supraglacial lake coverage (~770 km2) than the individual single-sensor products. [2]

maximum lake depth

Maximum lake depth and the proportion of lake area under the top of the metalimnion were the most important variables to predict the likelihood of hypolimnetic anoxia, which correctly predicted anoxic condition in 84% of lakes (Model 1). [1] Results Water temperature degree days and maximum lake depth were two leading predictors influencing both invasion risk and abundance, but they were relatively less important for predicting abundance than other water quality measures. [2] At the time of sampling in September 2017, the maximum lake depth was ~1 m. [3] However, bathymetric surveys conducted in October 2015 and September 2019 indicated that the maximum lake depth increased by 0. [4] Our study pushes back the timing of maximum lake depth at Lake George to at least MIS 3, rather than MIS 2. [5] We found evidence that thermal preferences influence how species9 depth use and biomass changed with lake size, proportion of littoral area, and maximum lake depth, although we found no relationship with lake shape. [6] Maximum lake depth and the presence of mixed fish communities (i. [7]

maximum lake level

Our results show that in 2016 lake level was the lowest of the past 44 years whereas the maximum lake level was recorded in 1985 (+11. [1] Annual series of peak discharge or maximum lake level, in agreement with previous studies, display increased frequency of floods in the mid-19th century and decreased frequency after the Second World War. [2] The Inle Lake record compares with Holocene sequences in China, Thailand and India and marine cores south of Myanmar, which similarly show a regional pattern of drier conditions in the early Greenlandian stage, followed by maximum lake levels in the early Northgrippian stage. [3]

maximum lake surface

Annual maximum lake surface temperature influences ecosystem structure and function and, in particular, the rates of metabolic activities, species survival and biogeography. [1] We carried out a quantitative analysis of and provided a discussion on the changes in the maximum lake surface water temperature (MLSWT) from 2001 to 2018 at two timescales (month and year) based on MODIS 11A2 composite product data and water temperature environment of cyanobacteria outbreaks. [2] The maximum lake surface area was 965. [3]

maximum lake evaporation

There was a ∼  5-month lag between the maximum net radiation (June) and maximum lake evaporation (November). [1] There was ~5 month lag between the maximum lake evaporation and maximum net radiation at Paiku Co. [2]

maximum lake extent

Besides, George VI Ice Shelf is analyzed for intra-annual lake dynamics throughout austral summer 2019/2020 and decision-level fused Sentinel-1 and Sentinel-2 maximum lake extent mapping products are presented for selected time periods. [1] In addition, George VI Ice Shelf is analyzed for intra-annual lake dynamics throughout austral summer 2019/2020 and a decision-level fused Sentinel-1 and Sentinel-2 maximum lake extent mapping product is presented for January 2020 revealing a more complete supraglacial lake coverage (~770 km2) than the individual single-sensor products. [2]