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2by Roser, C., Federici, S., Valentini, R., Montagnani, L., Schulze, -d, E., Mollicone, D., Kolle, O., Meroni, M., Papale, Dario, Belelli, L.Get access
Published 2002
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3by Papale, Dario, Roser, C., Montagnani, L., Schulze, -d, E., Mollicone, D., Kolle, O., Meroni, M., Belelli, L., Federici, S., Valentini, R.Get access
Published 2002
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4by Roser, C., Federici, S., Valentini, R., Montagnani, L., Schulze, -d, E., Mollicone, D., Kolle, O., Meroni, M., Papale, Dario, Belelli, L.Get access
Published in Tellus B (2002)
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5by Röser, C., Montagnani, L., Schulze, E., Mollicone, D., Kolle, O., Meroni, M., Papale, D., Marchesini, L., Federici, S., Valentini, R.“... daytime CO 2 exchange rates in July were -8.45 mumol m(-2) s(-1) in the Betula stand, -4.65 mumol m(-2...”
Published in Tellus B (2002)
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6by Carola Röser, Leonardo Montagnani, E.-Detlef Schulze, Danilo Mollicone, Olaf Kolle, Michele Meroni, Dario Papale, Luca Belelli Marchesini, Sandro Federici, Riccardo ValentiniGet access
Published in Tellus B: Chemical and Physical Meteorology (2002)
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7Net CO2 exchange rates in three different successional stages of the "Dark Taiga" of central Siberiaby ROSER, CAROLA, MONTAGNANI, LEONARDO, SCHULZE, E.-DETLEF, MOLLICONE, DANILO, KOLLE, OLAF, MERONI, MICHELE, PAPALE, DARIO, MARCHESINI, LUCA BELELLI, FEDERICI, SANDRO, VALENTINI, RICCARDOGet access
Published in Tellus B (2002)
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8by Biasi, Christina, Meyer, Hildegard, Rusalimova, Olga, Hämmerle, Rainer, Kaiser, Christina, Baranyi, Christian, Daims, Holger, Lashchinsky, Nikolaj, Barsukov, Pavel, Richter, AndreasGet access
Published in Plant and Soil (2008)
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9by Röser, Carola, Montagnani, Leonardo, Schulze, E.-Detlef, Mollicone, Danilo, Kolle, Olaf, Meroni, Michele, Papale, Dario, Marchesini, Luca Belelli, Federici, Sandro, Valentini, RiccardoGet access
Published in Tellus B: Chemical and Physical Meteorology (2002)
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10by Alekseychik, Pavel, Mammarella, Ivan, Karpov, Dmitry, Dengel, Sigrid, Terentieva, Irina, Sabrekov, Alexander, Glagolev, Mikhail, Lapshina, Elena“..., the surface exchange rates resembled those of pine-covered bogs elsewhere. The surface energy balance closure...”
Published in Atmospheric Chemistry and Physics (2018)
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11by P. Alekseychik, I. Mammarella, D. Karpov, S. Dengel, I. Terentieva, A. Sabrekov, M. Glagolev, E. Lapshina“..., the surface exchange rates resembled those of pine-covered bogs elsewhere. The surface energy balance closure...”
Published in Atmospheric Chemistry and Physics (2017)
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12by Alekseychik, Pavel, Mammarella, Ivan, Karpov, Dmitry, Dengel, Sigrid, Terentieva, Irina, Sabrekov, Alexander, Glagolev, Mikhail, Lapshina, Elena“..., the surface exchange rates resembled those of pine-covered bogs elsewhere. The surface energy balance closure...”
Published in Atmospheric Chemistry and Physics (2017)
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13by Juutinen, Sari, Aurela, Mika, Tuovinen, Juha-Pekka, Ivakhov, Viktor, Linkosalmi, Maiju, Räsänen, Aleksi, Virtanen, Tarmo, Mikola, Juha, Nyman, Johanna, Vähä, Emmi, Loskutova, Marina, Makshtas, Alexander, Laurila, Tuomas“..., had only small CO 2 exchange rates. While tundra wetlands were sources of CH 4 , lichen tundra...”
Published 2022
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14by Alekseychik, Pavel, Mammarella, Ivan, Karpov, Dmitry, Dengel, Sigrid, Terentieva, Irina, Sabrekov, Alexander, Glagolev, Mikhail, Lapshina, Elena“..., the surface exchange rates resembled those of pinecovered bogs elsewhere. The surface energy balance closure...”
Published in Atmospheric Chemistry and Physics (2017)
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15by Juutinen, Sari, Aurela, Mika, Tuovinen, Juha-Pekka, Ivakhov, Viktor, Linkosalmi, Maiju, Räsänen, Aleksi, Virtanen, Tarmo, Mikola, Juha, Nyman, Johanna, Vähä, Emmi, Loskutova, Marina, Makshtas, Alexander, Laurila, Tuomas“... exchange rates. The fens were the largest source of CH 4 , while the dry mineral soil tundra consumed...”
Published in Biogeosciences (2022)
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16by Juutinen, Sari, Aurela, Mika, Tuovinen, Juha-Pekka, Ivakhov, Viktor, Linkosalmi, Maiju, Räsänen, Aleksi, Virtanen, Tarmo, Mikola, Juha, Nyman, Johanna, Vähä, Emmi, Loskutova, Marina, Makshtas, Alexander, Laurila, Tuomas“... sequestration. Dry tundra, including the dwarf-shrub and lichen tundra, had smaller CO2 exchange rates. The fens...”
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17by S. Juutinen, M. Aurela, J.-P. Tuovinen, V. Ivakhov, M. Linkosalmi, A. Räsänen, T. Virtanen, J. Mikola, J. Nyman, E. Vähä, M. Loskutova, A. Makshtas, T. Laurila“... exchange rates. The fens were the largest source of CH 4 , while the dry mineral soil tundra consumed...”
Published in Biogeosciences (2022)
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18by Juutinen, Sari, Aurela, Mika, Tuovinen, Juha-Pekka, Ivakhov, Viktor, Linkosalmi, Maiju, Rasanen, Aleksi, Virtanen, Tarmo, Mikola, Juha, Nyman, Johanna, Vaha, Emmi, Loskutova, Marina, Makshtas, Alexander, Laurila, Tuomas“... exchange rates. The fens were the largest source of CH4, while the dry mineral soil tundra consumed...”
Published in Biogeosciences (2022)
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19by Henze, Adolf“... year by Breitkopf & Haertl of Leipzig. It answered the merchant's questions about exchange rates...”
Published 1891
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20by Henze, Adolf“... year by Breitkopf & Haertl of Leipzig. It answered the merchant's questions about exchange rates...”
Published 1891
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