Search

Your search keyword '"Stepanenko, Victor"' showing total 10 results
Start Over Author "Stepanenko, Victor" Publisher univ geneva, inst environm sci, geneva, switzerland.
10 results on '"Stepanenko, Victor"'

1. A framework for ensemble modelling of climate change impacts on lakes worldwide : the ISIMIP Lake Sector

Author

Golub, Malgorzata, Thiery, Wim, Marce, Rafael, Pierson, Don, Vanderkelen, Inne, Mercado-Bettin, Daniel, Woolway, R. Iestyn, Grant, Luke, Jennings, Eleanor, Kraemer, Benjamin M., Schewe, Jacob, Zhao, Fang, Frieler, Katja, Mengel, Matthias, Bogomolov, Vasiliy Y., Bouffard, Damien, Cote, Marianne, Couture, Raoul-Marie, Debolskiy, Andrey, V, Droppers, Bram, Gal, Gideon, Guo, Mingyang, Janssen, Annette B. G., Kirillin, Georgiy, Ladwig, Robert, Magee, Madeline, Moore, Tadhg, Perroud, Marjorie, Piccolroaz, Sebastiano, Vinnaa, Love Raaman, Schmid, Martin, Shatwell, Tom, Stepanenko, Victor M., Tan, Zeli, Woodward, Bronwyn, Yao, Huaxia, Adrian, Rita, Allan, Mathew, Anneville, Orlane, Arvola, Lauri, Atkins, Karen, Boegman, Leon, Carey, Cayelan, Christianson, Kyle, de Eyto, Elvira, DeGasperi, Curtis, Grechushnikova, Maria, Hejzlar, Josef, Joehnk, Klaus, Jones, Ian D., Laas, Alo, Mackay, Eleanor B., Mammarella, Ivan, Markensten, Hampus, McBride, Chris, Ozkundakci, Deniz, Potes, Miguel, Rinke, Karsten, Robertson, Dale, Rusak, James A., Salgado, Rui, van der Linden, Leon, Verburg, Piet, Wain, Danielle, Ward, Nicole K., Wollrab, Sabine, Zdorovennova, Galina, Golub, Malgorzata, Thiery, Wim, Marce, Rafael, Pierson, Don, Vanderkelen, Inne, Mercado-Bettin, Daniel, Woolway, R. Iestyn, Grant, Luke, Jennings, Eleanor, Kraemer, Benjamin M., Schewe, Jacob, Zhao, Fang, Frieler, Katja, Mengel, Matthias, Bogomolov, Vasiliy Y., Bouffard, Damien, Cote, Marianne, Couture, Raoul-Marie, Debolskiy, Andrey, V, Droppers, Bram, Gal, Gideon, Guo, Mingyang, Janssen, Annette B. G., Kirillin, Georgiy, Ladwig, Robert, Magee, Madeline, Moore, Tadhg, Perroud, Marjorie, Piccolroaz, Sebastiano, Vinnaa, Love Raaman, Schmid, Martin, Shatwell, Tom, Stepanenko, Victor M., Tan, Zeli, Woodward, Bronwyn, Yao, Huaxia, Adrian, Rita, Allan, Mathew, Anneville, Orlane, Arvola, Lauri, Atkins, Karen, Boegman, Leon, Carey, Cayelan, Christianson, Kyle, de Eyto, Elvira, DeGasperi, Curtis, Grechushnikova, Maria, Hejzlar, Josef, Joehnk, Klaus, Jones, Ian D., Laas, Alo, Mackay, Eleanor B., Mammarella, Ivan, Markensten, Hampus, McBride, Chris, Ozkundakci, Deniz, Potes, Miguel, Rinke, Karsten, Robertson, Dale, Rusak, James A., Salgado, Rui, van der Linden, Leon, Verburg, Piet, Wain, Danielle, Ward, Nicole K., Wollrab, Sabine, and Zdorovennova, Galina

Abstract

Empirical evidence demonstrates that lakes and reservoirs are warming across the globe. Consequently, there is an increased need to project future changes in lake thermal structure and resulting changes in lake biogeochemistry in order to plan for the likely impacts. Previous studies of the impacts of climate change on lakes have often relied on a single model forced with limited scenario-driven projections of future climate for a relatively small number of lakes. As a result, our understanding of the effects of climate change on lakes is fragmentary, based on scattered studies using different data sources and modelling protocols, and mainly focused on individual lakes or lake regions. This has precluded identification of the main impacts of climate change on lakes at global and regional scales and has likely contributed to the lack of lake water quality considerations in policy-relevant documents, such as the Assessment Reports of the Intergovernmental Panel on Climate Change (IPCC). Here, we describe a simulation protocol developed by the Lake Sector of the Inter-Sectoral Impact Model Intercomparison Project (ISIMIP) for simulating climate change impacts on lakes using an ensemble of lake models and climate change scenarios for ISIMIP phases 2 and 3. The protocol prescribes lake simulations driven by climate forcing from gridded observations and different Earth system models under various representative greenhouse gas concentration pathways (RCPs), all consistently bias-corrected on a 0.5 degrees x 0.5 degrees global grid. In ISIMIP phase 2, 11 lake models were forced with these data to project the thermal structure of 62 well-studied lakes where data were available for calibration under historical conditions, and using uncalibrated models for 17 500 lakes defined for all global grid cells containing lakes. In ISIMIP phase 3, this approach was expanded to consider more lakes, more models, and more processes. The ISIMIP Lake Sector is the largest international effo

Published
2022
Full Text
View/download PDF

2. A framework for ensemble modelling of climate change impacts on lakes worldwide : the ISIMIP Lake Sector

Author

Golub, Malgorzata, Thiery, Wim, Marce, Rafael, Pierson, Don, Vanderkelen, Inne, Mercado-Bettin, Daniel, Woolway, R. Iestyn, Grant, Luke, Jennings, Eleanor, Kraemer, Benjamin M., Schewe, Jacob, Zhao, Fang, Frieler, Katja, Mengel, Matthias, Bogomolov, Vasiliy Y., Bouffard, Damien, Cote, Marianne, Couture, Raoul-Marie, Debolskiy, Andrey, V, Droppers, Bram, Gal, Gideon, Guo, Mingyang, Janssen, Annette B. G., Kirillin, Georgiy, Ladwig, Robert, Magee, Madeline, Moore, Tadhg, Perroud, Marjorie, Piccolroaz, Sebastiano, Vinnaa, Love Raaman, Schmid, Martin, Shatwell, Tom, Stepanenko, Victor M., Tan, Zeli, Woodward, Bronwyn, Yao, Huaxia, Adrian, Rita, Allan, Mathew, Anneville, Orlane, Arvola, Lauri, Atkins, Karen, Boegman, Leon, Carey, Cayelan, Christianson, Kyle, de Eyto, Elvira, DeGasperi, Curtis, Grechushnikova, Maria, Hejzlar, Josef, Joehnk, Klaus, Jones, Ian D., Laas, Alo, Mackay, Eleanor B., Mammarella, Ivan, Markensten, Hampus, McBride, Chris, Ozkundakci, Deniz, Potes, Miguel, Rinke, Karsten, Robertson, Dale, Rusak, James A., Salgado, Rui, van der Linden, Leon, Verburg, Piet, Wain, Danielle, Ward, Nicole K., Wollrab, Sabine, Zdorovennova, Galina, Golub, Malgorzata, Thiery, Wim, Marce, Rafael, Pierson, Don, Vanderkelen, Inne, Mercado-Bettin, Daniel, Woolway, R. Iestyn, Grant, Luke, Jennings, Eleanor, Kraemer, Benjamin M., Schewe, Jacob, Zhao, Fang, Frieler, Katja, Mengel, Matthias, Bogomolov, Vasiliy Y., Bouffard, Damien, Cote, Marianne, Couture, Raoul-Marie, Debolskiy, Andrey, V, Droppers, Bram, Gal, Gideon, Guo, Mingyang, Janssen, Annette B. G., Kirillin, Georgiy, Ladwig, Robert, Magee, Madeline, Moore, Tadhg, Perroud, Marjorie, Piccolroaz, Sebastiano, Vinnaa, Love Raaman, Schmid, Martin, Shatwell, Tom, Stepanenko, Victor M., Tan, Zeli, Woodward, Bronwyn, Yao, Huaxia, Adrian, Rita, Allan, Mathew, Anneville, Orlane, Arvola, Lauri, Atkins, Karen, Boegman, Leon, Carey, Cayelan, Christianson, Kyle, de Eyto, Elvira, DeGasperi, Curtis, Grechushnikova, Maria, Hejzlar, Josef, Joehnk, Klaus, Jones, Ian D., Laas, Alo, Mackay, Eleanor B., Mammarella, Ivan, Markensten, Hampus, McBride, Chris, Ozkundakci, Deniz, Potes, Miguel, Rinke, Karsten, Robertson, Dale, Rusak, James A., Salgado, Rui, van der Linden, Leon, Verburg, Piet, Wain, Danielle, Ward, Nicole K., Wollrab, Sabine, and Zdorovennova, Galina

Abstract

Empirical evidence demonstrates that lakes and reservoirs are warming across the globe. Consequently, there is an increased need to project future changes in lake thermal structure and resulting changes in lake biogeochemistry in order to plan for the likely impacts. Previous studies of the impacts of climate change on lakes have often relied on a single model forced with limited scenario-driven projections of future climate for a relatively small number of lakes. As a result, our understanding of the effects of climate change on lakes is fragmentary, based on scattered studies using different data sources and modelling protocols, and mainly focused on individual lakes or lake regions. This has precluded identification of the main impacts of climate change on lakes at global and regional scales and has likely contributed to the lack of lake water quality considerations in policy-relevant documents, such as the Assessment Reports of the Intergovernmental Panel on Climate Change (IPCC). Here, we describe a simulation protocol developed by the Lake Sector of the Inter-Sectoral Impact Model Intercomparison Project (ISIMIP) for simulating climate change impacts on lakes using an ensemble of lake models and climate change scenarios for ISIMIP phases 2 and 3. The protocol prescribes lake simulations driven by climate forcing from gridded observations and different Earth system models under various representative greenhouse gas concentration pathways (RCPs), all consistently bias-corrected on a 0.5 degrees x 0.5 degrees global grid. In ISIMIP phase 2, 11 lake models were forced with these data to project the thermal structure of 62 well-studied lakes where data were available for calibration under historical conditions, and using uncalibrated models for 17 500 lakes defined for all global grid cells containing lakes. In ISIMIP phase 3, this approach was expanded to consider more lakes, more models, and more processes. The ISIMIP Lake Sector is the largest international effo

Published
2022
Full Text
View/download PDF

3. A framework for ensemble modelling of climate change impacts on lakes worldwide : the ISIMIP Lake Sector

Author

Golub, Malgorzata, Thiery, Wim, Marce, Rafael, Pierson, Don, Vanderkelen, Inne, Mercado-Bettin, Daniel, Woolway, R. Iestyn, Grant, Luke, Jennings, Eleanor, Kraemer, Benjamin M., Schewe, Jacob, Zhao, Fang, Frieler, Katja, Mengel, Matthias, Bogomolov, Vasiliy Y., Bouffard, Damien, Cote, Marianne, Couture, Raoul-Marie, Debolskiy, Andrey, V, Droppers, Bram, Gal, Gideon, Guo, Mingyang, Janssen, Annette B. G., Kirillin, Georgiy, Ladwig, Robert, Magee, Madeline, Moore, Tadhg, Perroud, Marjorie, Piccolroaz, Sebastiano, Vinnaa, Love Raaman, Schmid, Martin, Shatwell, Tom, Stepanenko, Victor M., Tan, Zeli, Woodward, Bronwyn, Yao, Huaxia, Adrian, Rita, Allan, Mathew, Anneville, Orlane, Arvola, Lauri, Atkins, Karen, Boegman, Leon, Carey, Cayelan, Christianson, Kyle, de Eyto, Elvira, DeGasperi, Curtis, Grechushnikova, Maria, Hejzlar, Josef, Joehnk, Klaus, Jones, Ian D., Laas, Alo, Mackay, Eleanor B., Mammarella, Ivan, Markensten, Hampus, McBride, Chris, Ozkundakci, Deniz, Potes, Miguel, Rinke, Karsten, Robertson, Dale, Rusak, James A., Salgado, Rui, van der Linden, Leon, Verburg, Piet, Wain, Danielle, Ward, Nicole K., Wollrab, Sabine, Zdorovennova, Galina, Golub, Malgorzata, Thiery, Wim, Marce, Rafael, Pierson, Don, Vanderkelen, Inne, Mercado-Bettin, Daniel, Woolway, R. Iestyn, Grant, Luke, Jennings, Eleanor, Kraemer, Benjamin M., Schewe, Jacob, Zhao, Fang, Frieler, Katja, Mengel, Matthias, Bogomolov, Vasiliy Y., Bouffard, Damien, Cote, Marianne, Couture, Raoul-Marie, Debolskiy, Andrey, V, Droppers, Bram, Gal, Gideon, Guo, Mingyang, Janssen, Annette B. G., Kirillin, Georgiy, Ladwig, Robert, Magee, Madeline, Moore, Tadhg, Perroud, Marjorie, Piccolroaz, Sebastiano, Vinnaa, Love Raaman, Schmid, Martin, Shatwell, Tom, Stepanenko, Victor M., Tan, Zeli, Woodward, Bronwyn, Yao, Huaxia, Adrian, Rita, Allan, Mathew, Anneville, Orlane, Arvola, Lauri, Atkins, Karen, Boegman, Leon, Carey, Cayelan, Christianson, Kyle, de Eyto, Elvira, DeGasperi, Curtis, Grechushnikova, Maria, Hejzlar, Josef, Joehnk, Klaus, Jones, Ian D., Laas, Alo, Mackay, Eleanor B., Mammarella, Ivan, Markensten, Hampus, McBride, Chris, Ozkundakci, Deniz, Potes, Miguel, Rinke, Karsten, Robertson, Dale, Rusak, James A., Salgado, Rui, van der Linden, Leon, Verburg, Piet, Wain, Danielle, Ward, Nicole K., Wollrab, Sabine, and Zdorovennova, Galina

Abstract

Empirical evidence demonstrates that lakes and reservoirs are warming across the globe. Consequently, there is an increased need to project future changes in lake thermal structure and resulting changes in lake biogeochemistry in order to plan for the likely impacts. Previous studies of the impacts of climate change on lakes have often relied on a single model forced with limited scenario-driven projections of future climate for a relatively small number of lakes. As a result, our understanding of the effects of climate change on lakes is fragmentary, based on scattered studies using different data sources and modelling protocols, and mainly focused on individual lakes or lake regions. This has precluded identification of the main impacts of climate change on lakes at global and regional scales and has likely contributed to the lack of lake water quality considerations in policy-relevant documents, such as the Assessment Reports of the Intergovernmental Panel on Climate Change (IPCC). Here, we describe a simulation protocol developed by the Lake Sector of the Inter-Sectoral Impact Model Intercomparison Project (ISIMIP) for simulating climate change impacts on lakes using an ensemble of lake models and climate change scenarios for ISIMIP phases 2 and 3. The protocol prescribes lake simulations driven by climate forcing from gridded observations and different Earth system models under various representative greenhouse gas concentration pathways (RCPs), all consistently bias-corrected on a 0.5 degrees x 0.5 degrees global grid. In ISIMIP phase 2, 11 lake models were forced with these data to project the thermal structure of 62 well-studied lakes where data were available for calibration under historical conditions, and using uncalibrated models for 17 500 lakes defined for all global grid cells containing lakes. In ISIMIP phase 3, this approach was expanded to consider more lakes, more models, and more processes. The ISIMIP Lake Sector is the largest international effo

Published
2022
Full Text
View/download PDF

4. A framework for ensemble modelling of climate change impacts on lakes worldwide : the ISIMIP Lake Sector

Author

Golub, Malgorzata, Thiery, Wim, Marce, Rafael, Pierson, Don, Vanderkelen, Inne, Mercado-Bettin, Daniel, Woolway, R. Iestyn, Grant, Luke, Jennings, Eleanor, Kraemer, Benjamin M., Schewe, Jacob, Zhao, Fang, Frieler, Katja, Mengel, Matthias, Bogomolov, Vasiliy Y., Bouffard, Damien, Cote, Marianne, Couture, Raoul-Marie, Debolskiy, Andrey, V, Droppers, Bram, Gal, Gideon, Guo, Mingyang, Janssen, Annette B. G., Kirillin, Georgiy, Ladwig, Robert, Magee, Madeline, Moore, Tadhg, Perroud, Marjorie, Piccolroaz, Sebastiano, Vinnaa, Love Raaman, Schmid, Martin, Shatwell, Tom, Stepanenko, Victor M., Tan, Zeli, Woodward, Bronwyn, Yao, Huaxia, Adrian, Rita, Allan, Mathew, Anneville, Orlane, Arvola, Lauri, Atkins, Karen, Boegman, Leon, Carey, Cayelan, Christianson, Kyle, de Eyto, Elvira, DeGasperi, Curtis, Grechushnikova, Maria, Hejzlar, Josef, Joehnk, Klaus, Jones, Ian D., Laas, Alo, Mackay, Eleanor B., Mammarella, Ivan, Markensten, Hampus, McBride, Chris, Ozkundakci, Deniz, Potes, Miguel, Rinke, Karsten, Robertson, Dale, Rusak, James A., Salgado, Rui, van der Linden, Leon, Verburg, Piet, Wain, Danielle, Ward, Nicole K., Wollrab, Sabine, Zdorovennova, Galina, Golub, Malgorzata, Thiery, Wim, Marce, Rafael, Pierson, Don, Vanderkelen, Inne, Mercado-Bettin, Daniel, Woolway, R. Iestyn, Grant, Luke, Jennings, Eleanor, Kraemer, Benjamin M., Schewe, Jacob, Zhao, Fang, Frieler, Katja, Mengel, Matthias, Bogomolov, Vasiliy Y., Bouffard, Damien, Cote, Marianne, Couture, Raoul-Marie, Debolskiy, Andrey, V, Droppers, Bram, Gal, Gideon, Guo, Mingyang, Janssen, Annette B. G., Kirillin, Georgiy, Ladwig, Robert, Magee, Madeline, Moore, Tadhg, Perroud, Marjorie, Piccolroaz, Sebastiano, Vinnaa, Love Raaman, Schmid, Martin, Shatwell, Tom, Stepanenko, Victor M., Tan, Zeli, Woodward, Bronwyn, Yao, Huaxia, Adrian, Rita, Allan, Mathew, Anneville, Orlane, Arvola, Lauri, Atkins, Karen, Boegman, Leon, Carey, Cayelan, Christianson, Kyle, de Eyto, Elvira, DeGasperi, Curtis, Grechushnikova, Maria, Hejzlar, Josef, Joehnk, Klaus, Jones, Ian D., Laas, Alo, Mackay, Eleanor B., Mammarella, Ivan, Markensten, Hampus, McBride, Chris, Ozkundakci, Deniz, Potes, Miguel, Rinke, Karsten, Robertson, Dale, Rusak, James A., Salgado, Rui, van der Linden, Leon, Verburg, Piet, Wain, Danielle, Ward, Nicole K., Wollrab, Sabine, and Zdorovennova, Galina

Abstract

Empirical evidence demonstrates that lakes and reservoirs are warming across the globe. Consequently, there is an increased need to project future changes in lake thermal structure and resulting changes in lake biogeochemistry in order to plan for the likely impacts. Previous studies of the impacts of climate change on lakes have often relied on a single model forced with limited scenario-driven projections of future climate for a relatively small number of lakes. As a result, our understanding of the effects of climate change on lakes is fragmentary, based on scattered studies using different data sources and modelling protocols, and mainly focused on individual lakes or lake regions. This has precluded identification of the main impacts of climate change on lakes at global and regional scales and has likely contributed to the lack of lake water quality considerations in policy-relevant documents, such as the Assessment Reports of the Intergovernmental Panel on Climate Change (IPCC). Here, we describe a simulation protocol developed by the Lake Sector of the Inter-Sectoral Impact Model Intercomparison Project (ISIMIP) for simulating climate change impacts on lakes using an ensemble of lake models and climate change scenarios for ISIMIP phases 2 and 3. The protocol prescribes lake simulations driven by climate forcing from gridded observations and different Earth system models under various representative greenhouse gas concentration pathways (RCPs), all consistently bias-corrected on a 0.5 degrees x 0.5 degrees global grid. In ISIMIP phase 2, 11 lake models were forced with these data to project the thermal structure of 62 well-studied lakes where data were available for calibration under historical conditions, and using uncalibrated models for 17 500 lakes defined for all global grid cells containing lakes. In ISIMIP phase 3, this approach was expanded to consider more lakes, more models, and more processes. The ISIMIP Lake Sector is the largest international effo

Published
2022
Full Text
View/download PDF

5. A framework for ensemble modelling of climate change impacts on lakes worldwide : the ISIMIP Lake Sector

Author

Golub, Malgorzata, Thiery, Wim, Marce, Rafael, Pierson, Don, Vanderkelen, Inne, Mercado-Bettin, Daniel, Woolway, R. Iestyn, Grant, Luke, Jennings, Eleanor, Kraemer, Benjamin M., Schewe, Jacob, Zhao, Fang, Frieler, Katja, Mengel, Matthias, Bogomolov, Vasiliy Y., Bouffard, Damien, Cote, Marianne, Couture, Raoul-Marie, Debolskiy, Andrey, V, Droppers, Bram, Gal, Gideon, Guo, Mingyang, Janssen, Annette B. G., Kirillin, Georgiy, Ladwig, Robert, Magee, Madeline, Moore, Tadhg, Perroud, Marjorie, Piccolroaz, Sebastiano, Vinnaa, Love Raaman, Schmid, Martin, Shatwell, Tom, Stepanenko, Victor M., Tan, Zeli, Woodward, Bronwyn, Yao, Huaxia, Adrian, Rita, Allan, Mathew, Anneville, Orlane, Arvola, Lauri, Atkins, Karen, Boegman, Leon, Carey, Cayelan, Christianson, Kyle, de Eyto, Elvira, DeGasperi, Curtis, Grechushnikova, Maria, Hejzlar, Josef, Joehnk, Klaus, Jones, Ian D., Laas, Alo, Mackay, Eleanor B., Mammarella, Ivan, Markensten, Hampus, McBride, Chris, Ozkundakci, Deniz, Potes, Miguel, Rinke, Karsten, Robertson, Dale, Rusak, James A., Salgado, Rui, van der Linden, Leon, Verburg, Piet, Wain, Danielle, Ward, Nicole K., Wollrab, Sabine, Zdorovennova, Galina, Golub, Malgorzata, Thiery, Wim, Marce, Rafael, Pierson, Don, Vanderkelen, Inne, Mercado-Bettin, Daniel, Woolway, R. Iestyn, Grant, Luke, Jennings, Eleanor, Kraemer, Benjamin M., Schewe, Jacob, Zhao, Fang, Frieler, Katja, Mengel, Matthias, Bogomolov, Vasiliy Y., Bouffard, Damien, Cote, Marianne, Couture, Raoul-Marie, Debolskiy, Andrey, V, Droppers, Bram, Gal, Gideon, Guo, Mingyang, Janssen, Annette B. G., Kirillin, Georgiy, Ladwig, Robert, Magee, Madeline, Moore, Tadhg, Perroud, Marjorie, Piccolroaz, Sebastiano, Vinnaa, Love Raaman, Schmid, Martin, Shatwell, Tom, Stepanenko, Victor M., Tan, Zeli, Woodward, Bronwyn, Yao, Huaxia, Adrian, Rita, Allan, Mathew, Anneville, Orlane, Arvola, Lauri, Atkins, Karen, Boegman, Leon, Carey, Cayelan, Christianson, Kyle, de Eyto, Elvira, DeGasperi, Curtis, Grechushnikova, Maria, Hejzlar, Josef, Joehnk, Klaus, Jones, Ian D., Laas, Alo, Mackay, Eleanor B., Mammarella, Ivan, Markensten, Hampus, McBride, Chris, Ozkundakci, Deniz, Potes, Miguel, Rinke, Karsten, Robertson, Dale, Rusak, James A., Salgado, Rui, van der Linden, Leon, Verburg, Piet, Wain, Danielle, Ward, Nicole K., Wollrab, Sabine, and Zdorovennova, Galina

Abstract

Empirical evidence demonstrates that lakes and reservoirs are warming across the globe. Consequently, there is an increased need to project future changes in lake thermal structure and resulting changes in lake biogeochemistry in order to plan for the likely impacts. Previous studies of the impacts of climate change on lakes have often relied on a single model forced with limited scenario-driven projections of future climate for a relatively small number of lakes. As a result, our understanding of the effects of climate change on lakes is fragmentary, based on scattered studies using different data sources and modelling protocols, and mainly focused on individual lakes or lake regions. This has precluded identification of the main impacts of climate change on lakes at global and regional scales and has likely contributed to the lack of lake water quality considerations in policy-relevant documents, such as the Assessment Reports of the Intergovernmental Panel on Climate Change (IPCC). Here, we describe a simulation protocol developed by the Lake Sector of the Inter-Sectoral Impact Model Intercomparison Project (ISIMIP) for simulating climate change impacts on lakes using an ensemble of lake models and climate change scenarios for ISIMIP phases 2 and 3. The protocol prescribes lake simulations driven by climate forcing from gridded observations and different Earth system models under various representative greenhouse gas concentration pathways (RCPs), all consistently bias-corrected on a 0.5 degrees x 0.5 degrees global grid. In ISIMIP phase 2, 11 lake models were forced with these data to project the thermal structure of 62 well-studied lakes where data were available for calibration under historical conditions, and using uncalibrated models for 17 500 lakes defined for all global grid cells containing lakes. In ISIMIP phase 3, this approach was expanded to consider more lakes, more models, and more processes. The ISIMIP Lake Sector is the largest international effo

Published
2022
Full Text
View/download PDF

6. Phenological shifts in lake stratification under climate change

Author

Woolway, R. Iestyn, Sharma, Sapna, Weyhenmeyer, Gesa A., Debolskiy, Andrey, Golub, Malgorzata, Mercado-Bettin, Daniel, Perroud, Marjorie, Stepanenko, Victor, Tan, Zeli, Grant, Luke, Ladwig, Robert, Mesman, Jorrit P., Moore, Tadhg N., Shatwell, Tom, Vanderkelen, Inne, Austin, Jay A., DeGasperi, Curtis L., Dokulil, Martin, La Fuente, Sofia, Mackay, Eleanor B., Schladow, S. Geoffrey, Watanabe, Shohei, Marce, Rafael, Pierson, Don, Thiery, Wim, Jennings, Eleanor, Woolway, R. Iestyn, Sharma, Sapna, Weyhenmeyer, Gesa A., Debolskiy, Andrey, Golub, Malgorzata, Mercado-Bettin, Daniel, Perroud, Marjorie, Stepanenko, Victor, Tan, Zeli, Grant, Luke, Ladwig, Robert, Mesman, Jorrit P., Moore, Tadhg N., Shatwell, Tom, Vanderkelen, Inne, Austin, Jay A., DeGasperi, Curtis L., Dokulil, Martin, La Fuente, Sofia, Mackay, Eleanor B., Schladow, S. Geoffrey, Watanabe, Shohei, Marce, Rafael, Pierson, Don, Thiery, Wim, and Jennings, Eleanor

Abstract

One of the most important physical characteristics driving lifecycle events in lakes is stratification. Already subtle variations in the timing of stratification onset and break-up (phenology) are known to have major ecological effects, mainly by determining the availability of light, nutrients, carbon and oxygen to organisms. Despite its ecological importance, historic and future global changes in stratification phenology are unknown. Here, we used a lake-climate model ensemble and long-term observational data, to investigate changes in lake stratification phenology across the Northern Hemisphere from 1901 to 2099. Under the high-greenhouse-gas-emission scenario, stratification will begin 22.0 +/- 7.0 days earlier and end 11.3 +/- 4.7 days later by the end of this century. It is very likely that this 33.3 +/- 11.7 day prolongation in stratification will accelerate lake deoxygenation with subsequent effects on nutrient mineralization and phosphorus release from lake sediments. Further misalignment of lifecycle events, with possible irreversible changes for lake ecosystems, is also likely.

Published
2021
Full Text
View/download PDF

7. Phenological shifts in lake stratification under climate change

Author

Woolway, R. Iestyn, Sharma, Sapna, Weyhenmeyer, Gesa A., Debolskiy, Andrey, Golub, Malgorzata, Mercado-Bettin, Daniel, Perroud, Marjorie, Stepanenko, Victor, Tan, Zeli, Grant, Luke, Ladwig, Robert, Mesman, Jorrit P., Moore, Tadhg N., Shatwell, Tom, Vanderkelen, Inne, Austin, Jay A., DeGasperi, Curtis L., Dokulil, Martin, La Fuente, Sofia, Mackay, Eleanor B., Schladow, S. Geoffrey, Watanabe, Shohei, Marce, Rafael, Pierson, Don, Thiery, Wim, Jennings, Eleanor, Woolway, R. Iestyn, Sharma, Sapna, Weyhenmeyer, Gesa A., Debolskiy, Andrey, Golub, Malgorzata, Mercado-Bettin, Daniel, Perroud, Marjorie, Stepanenko, Victor, Tan, Zeli, Grant, Luke, Ladwig, Robert, Mesman, Jorrit P., Moore, Tadhg N., Shatwell, Tom, Vanderkelen, Inne, Austin, Jay A., DeGasperi, Curtis L., Dokulil, Martin, La Fuente, Sofia, Mackay, Eleanor B., Schladow, S. Geoffrey, Watanabe, Shohei, Marce, Rafael, Pierson, Don, Thiery, Wim, and Jennings, Eleanor

Abstract

One of the most important physical characteristics driving lifecycle events in lakes is stratification. Already subtle variations in the timing of stratification onset and break-up (phenology) are known to have major ecological effects, mainly by determining the availability of light, nutrients, carbon and oxygen to organisms. Despite its ecological importance, historic and future global changes in stratification phenology are unknown. Here, we used a lake-climate model ensemble and long-term observational data, to investigate changes in lake stratification phenology across the Northern Hemisphere from 1901 to 2099. Under the high-greenhouse-gas-emission scenario, stratification will begin 22.0 +/- 7.0 days earlier and end 11.3 +/- 4.7 days later by the end of this century. It is very likely that this 33.3 +/- 11.7 day prolongation in stratification will accelerate lake deoxygenation with subsequent effects on nutrient mineralization and phosphorus release from lake sediments. Further misalignment of lifecycle events, with possible irreversible changes for lake ecosystems, is also likely.

Published
2021
Full Text
View/download PDF

8. Phenological shifts in lake stratification under climate change

Author

Woolway, R. Iestyn, Sharma, Sapna, Weyhenmeyer, Gesa A., Debolskiy, Andrey, Golub, Malgorzata, Mercado-Bettin, Daniel, Perroud, Marjorie, Stepanenko, Victor, Tan, Zeli, Grant, Luke, Ladwig, Robert, Mesman, Jorrit P., Moore, Tadhg N., Shatwell, Tom, Vanderkelen, Inne, Austin, Jay A., DeGasperi, Curtis L., Dokulil, Martin, La Fuente, Sofia, Mackay, Eleanor B., Schladow, S. Geoffrey, Watanabe, Shohei, Marce, Rafael, Pierson, Don, Thiery, Wim, Jennings, Eleanor, Woolway, R. Iestyn, Sharma, Sapna, Weyhenmeyer, Gesa A., Debolskiy, Andrey, Golub, Malgorzata, Mercado-Bettin, Daniel, Perroud, Marjorie, Stepanenko, Victor, Tan, Zeli, Grant, Luke, Ladwig, Robert, Mesman, Jorrit P., Moore, Tadhg N., Shatwell, Tom, Vanderkelen, Inne, Austin, Jay A., DeGasperi, Curtis L., Dokulil, Martin, La Fuente, Sofia, Mackay, Eleanor B., Schladow, S. Geoffrey, Watanabe, Shohei, Marce, Rafael, Pierson, Don, Thiery, Wim, and Jennings, Eleanor

Abstract

One of the most important physical characteristics driving lifecycle events in lakes is stratification. Already subtle variations in the timing of stratification onset and break-up (phenology) are known to have major ecological effects, mainly by determining the availability of light, nutrients, carbon and oxygen to organisms. Despite its ecological importance, historic and future global changes in stratification phenology are unknown. Here, we used a lake-climate model ensemble and long-term observational data, to investigate changes in lake stratification phenology across the Northern Hemisphere from 1901 to 2099. Under the high-greenhouse-gas-emission scenario, stratification will begin 22.0 +/- 7.0 days earlier and end 11.3 +/- 4.7 days later by the end of this century. It is very likely that this 33.3 +/- 11.7 day prolongation in stratification will accelerate lake deoxygenation with subsequent effects on nutrient mineralization and phosphorus release from lake sediments. Further misalignment of lifecycle events, with possible irreversible changes for lake ecosystems, is also likely.

Published
2021
Full Text
View/download PDF

9. Phenological shifts in lake stratification under climate change

Author

Woolway, R. Iestyn, Sharma, Sapna, Weyhenmeyer, Gesa A., Debolskiy, Andrey, Golub, Malgorzata, Mercado-Bettin, Daniel, Perroud, Marjorie, Stepanenko, Victor, Tan, Zeli, Grant, Luke, Ladwig, Robert, Mesman, Jorrit P., Moore, Tadhg N., Shatwell, Tom, Vanderkelen, Inne, Austin, Jay A., DeGasperi, Curtis L., Dokulil, Martin, La Fuente, Sofia, Mackay, Eleanor B., Schladow, S. Geoffrey, Watanabe, Shohei, Marce, Rafael, Pierson, Don, Thiery, Wim, Jennings, Eleanor, Woolway, R. Iestyn, Sharma, Sapna, Weyhenmeyer, Gesa A., Debolskiy, Andrey, Golub, Malgorzata, Mercado-Bettin, Daniel, Perroud, Marjorie, Stepanenko, Victor, Tan, Zeli, Grant, Luke, Ladwig, Robert, Mesman, Jorrit P., Moore, Tadhg N., Shatwell, Tom, Vanderkelen, Inne, Austin, Jay A., DeGasperi, Curtis L., Dokulil, Martin, La Fuente, Sofia, Mackay, Eleanor B., Schladow, S. Geoffrey, Watanabe, Shohei, Marce, Rafael, Pierson, Don, Thiery, Wim, and Jennings, Eleanor

Abstract

One of the most important physical characteristics driving lifecycle events in lakes is stratification. Already subtle variations in the timing of stratification onset and break-up (phenology) are known to have major ecological effects, mainly by determining the availability of light, nutrients, carbon and oxygen to organisms. Despite its ecological importance, historic and future global changes in stratification phenology are unknown. Here, we used a lake-climate model ensemble and long-term observational data, to investigate changes in lake stratification phenology across the Northern Hemisphere from 1901 to 2099. Under the high-greenhouse-gas-emission scenario, stratification will begin 22.0 +/- 7.0 days earlier and end 11.3 +/- 4.7 days later by the end of this century. It is very likely that this 33.3 +/- 11.7 day prolongation in stratification will accelerate lake deoxygenation with subsequent effects on nutrient mineralization and phosphorus release from lake sediments. Further misalignment of lifecycle events, with possible irreversible changes for lake ecosystems, is also likely.

Published
2021
Full Text
View/download PDF

10. Phenological shifts in lake stratification under climate change

Author

Woolway, R. Iestyn, Sharma, Sapna, Weyhenmeyer, Gesa A., Debolskiy, Andrey, Golub, Malgorzata, Mercado-Bettin, Daniel, Perroud, Marjorie, Stepanenko, Victor, Tan, Zeli, Grant, Luke, Ladwig, Robert, Mesman, Jorrit P., Moore, Tadhg N., Shatwell, Tom, Vanderkelen, Inne, Austin, Jay A., DeGasperi, Curtis L., Dokulil, Martin, La Fuente, Sofia, Mackay, Eleanor B., Schladow, S. Geoffrey, Watanabe, Shohei, Marce, Rafael, Pierson, Don, Thiery, Wim, Jennings, Eleanor, Woolway, R. Iestyn, Sharma, Sapna, Weyhenmeyer, Gesa A., Debolskiy, Andrey, Golub, Malgorzata, Mercado-Bettin, Daniel, Perroud, Marjorie, Stepanenko, Victor, Tan, Zeli, Grant, Luke, Ladwig, Robert, Mesman, Jorrit P., Moore, Tadhg N., Shatwell, Tom, Vanderkelen, Inne, Austin, Jay A., DeGasperi, Curtis L., Dokulil, Martin, La Fuente, Sofia, Mackay, Eleanor B., Schladow, S. Geoffrey, Watanabe, Shohei, Marce, Rafael, Pierson, Don, Thiery, Wim, and Jennings, Eleanor

Abstract

One of the most important physical characteristics driving lifecycle events in lakes is stratification. Already subtle variations in the timing of stratification onset and break-up (phenology) are known to have major ecological effects, mainly by determining the availability of light, nutrients, carbon and oxygen to organisms. Despite its ecological importance, historic and future global changes in stratification phenology are unknown. Here, we used a lake-climate model ensemble and long-term observational data, to investigate changes in lake stratification phenology across the Northern Hemisphere from 1901 to 2099. Under the high-greenhouse-gas-emission scenario, stratification will begin 22.0 +/- 7.0 days earlier and end 11.3 +/- 4.7 days later by the end of this century. It is very likely that this 33.3 +/- 11.7 day prolongation in stratification will accelerate lake deoxygenation with subsequent effects on nutrient mineralization and phosphorus release from lake sediments. Further misalignment of lifecycle events, with possible irreversible changes for lake ecosystems, is also likely.

Published
2021
Full Text
View/download PDF

Catalog

Books, media, physical & digital resources
See catalog results